Studies on the toxic effects of selected heavy metals in the freshwater mussel lamellidens corrianus (lea)

Industrialisation affects air, water, and soil. Industrial effluents which enter the aquatic environment either by direct disposal or through run off, affect living organisms at morphological and physiological levels. In any living tissue toxic materials exert their effects first at molecular and biochemical levels (Robbins and Angell, 1976). Most of the industrial effluents contain elevated concentrations of organic and inorganic chemicals capable of eliciting stimulatory or inhibitory effects on the metabolism of aquatic organisms. Heavy metals form an important group of environmental pollutants. Effects of pollution on the aquatic environment by heavy metals have received considerable attention in recent years due to their toxicity even at very low levels, persistence in the environment, and chances of getting biomagnified. A pollutant that does not affect a particular process under normal unstressed condition may affect the ability of the animal to adjust to changing environmental conditions which ultimately decrease its chances of survival (Thurberg et al., 1973

Source Characterization of Sedimentary Organic Matter in a Tropical Estuary, Southwest Coast of India: A Biomarker Approach

The source, fate and diagentic pathway of sedimentary organic matter in estuaries are difficult to delineate due to the complexity of organic matter sources, intensive physical mixing and biological processes. A combination of bulk organic matter techniques and molecular biomarkers are found to be successful in explaining organic matter dynamics in estuaries. The basic requirement for these multi-proxy approaches are (i) sources have significantly differing characteristics, (ii) there are a sufficient number of tracers to delineate all sources and (iii) organic matter degradation and processing have little, similar or predictable effects on end member characteristics. Although there have been abundant researches that have attempted to tackle difficulties related to the source and fate of organic matter in estuarine systems, our understanding remains limited or rather inconsistent regarding the Indian estuaries. Cochin estuary is the largest among many extensive estuarine systems along the southwest coast of India. It supports as much biological productivity and diversity as tropical rain forests. In this study, we have used a combination of bulk geochemical parameters and different group of molecular biomarkers to define organic matter sources and thereby identifying various biogeochemical processes acting along the salinity gradient of the Cochin estuary

" Studies on Laser induced Phatothermal Phenomena in Selected Organic Compounds and Fullerenes"

In the pre—laser era it was difficult to believe that the optical properties of a medium depend upon the intensity of the radiation incident on it. The basis for this conclusion is that the electric field strength associated with the conventional light sources used before the advent of lasers was much smaller than (103 V/cm) the field sttrengths of atomic or interatomic fields (2 107 —- 10” V/cm). The radiation with such low intensity is not able to affect atomic fields to the extent of changing optical parameters. The invention of laser in 1960 was a turning point. The high degree of coherence of the laser radiation provides high spatial concentration of optical power. With the availability of the femtosecond lasers it has become possible to get extremely high peak powers 2 1013 W/cmz). At such high fields, the relationship between electric ‘polarization P and the electric field strength E ceases to be linear and several nonlinear effects begin to occur. Nonlinear absorption, a branch of nonlinear optics, refers to the interaction between radiation and matter accompanied by absorption of more than one photon. Nonlinear absorption has acquired great importance after the invention of high power lasers. One of the objectives of the present work is to investigate the nonlinear absorption processes occurring in fullerene, selected organic solvents and laser dyes. Fullerenes and laser dyes were chosen because of their highly nonlinear behaviour. Fullerenes, the most beautiful among molecules, offer fascinating field of research owinglto their significant structural properties. As toluene, benzene and carbon disulphide are themost widely used solvents for fullerenes, it seems important to study the nonlinear properties of these liquids as well. Like fullerenes, laser dyes also possess highly delocalized 7r electrons which are responsible for their nonlinear absorption. Dye lasers were the fulfillment of an experimenter’s pipe dream - to have a laser that is easily tunable over a wide range of wavelengths. A better understandingof the photophysical properties of laser dyes can significantly enhance the development and technology of dye lasers. We studied the nonlinear absorption properties of two rhodamine dyes to have some insight into their nonlinear optical properties.

Synthesis, Characterization and Applications of Modified TiO2 Systems

This thesis is divided in to 9 chapters and deals with the modification of TiO2 for various applications include photocatalysis, thermal reaction, photovoltaics and non-linear optics. Chapter 1 involves a brief introduction of the topic of study. An introduction to the applications of modified titania systems in various fields are discussed concisely. Scope and objectives of the present work are also discussed in this chapter. Chapter 2 explains the strategy adopted for the synthesis of metal, nonmetal co-doped TiO2 systems. Hydrothermal technique was employed for the preparation of the co-doped TiO2 system, where Ti[OCH(CH3)2]4, urea and metal nitrates were used as the sources for TiO2, N and metals respectively. In all the co-doped systems, urea to Ti[OCH(CH3)2]4 was taken in a 1:1 molar ratio and varied the concentration of metals. Five different co-doped catalytic systems and for each catalysts, three versions were prepared by varying the concentration of metals. A brief explanation of physico-chemical techniques used for the characterization of the material was also presented in this chapter. This includes X-ray Diffraction (XRD), Raman Spectroscopy, FTIR analysis, Thermo Gravimetric Analysis, Energy Dispersive X-ray Analysis (EDX), Scanning Electron Microscopy(SEM), UV-Visible Diffuse Reflectance Spectroscopy (UV-Vis DRS), Transmission Electron Microscopy (TEM), BET Surface Area Measurements and X-ray Photoelectron Spectroscopy (XPS). Chapter 3 contains the results and discussion of characterization techniques used for analyzing the prepared systems. Characterization is an inevitable part of materials research. Determination of physico-chemical properties of the prepared materials using suitable characterization techniques is very crucial to find its exact field of application. It is clear from the XRD pattern that photocatalytically active anatase phase dominates in the calcined samples with peaks at 2θ values around 25.4°, 38°, 48.1°, 55.2° and 62.7° corresponding to (101), (004), (200), (211) and (204) crystal planes (JCPDS 21-1272) respectively. But in the case of Pr-N-Ti sample, a new peak was observed at 2θ = 30.8° corresponding to the (121) plane of the polymorph brookite. There are no visible peaks corresponding to dopants, which may be due to their low concentration or it is an indication of the better dispersion of impurities in the TiO2. Crystallite size of the sample was calculated from Scherrer equation byusing full width at half maximum (FWHM) of the (101) peak of the anatase phase. Crystallite size of all the co-doped TiO2 was found to be lower than that of bare TiO2 which indicates that the doping of metal ions having higher ionic radius into the lattice of TiO2 causes some lattice distortion which suppress the growth of TiO2 nanoparticles. The structural identity of the prepared system obtained from XRD pattern is further confirmed by Raman spectra measurements. Anatase has six Raman active modes. Band gap of the co-doped system was calculated using Kubelka-Munk equation and that was found to be lower than pure TiO2. Stability of the prepared systems was understood from thermo gravimetric analysis. FT-IR was performed to understand the functional groups as well as to study the surface changes occurred during modification. EDX was used to determine the impurities present in the system. The EDX spectra of all the co-doped samples show signals directly related to the dopants. Spectra of all the co-doped systems contain O and Ti as the main components with low concentrations of doped elements. Morphologies of the prepared systems were obtained from SEM and TEM analysis. Average particle size of the systems was drawn from histogram data. Electronic structures of the samples were identified perfectly from XPS measurements. Chapter 4 describes the photocatalytic degradation of herbicides Atrazine and Metolachlor using metal, non-metal co-doped titania systems. The percentage of degradation was analyzed by HPLC technique. Parameters such as effect of different catalysts, effect of time, effect of catalysts amount and reusability studies were discussed. Chapter 5 deals with the photo-oxidation of some anthracene derivatives by co-doped catalytic systems. These anthracene derivatives come underthe category of polycyclic aromatic hydrocarbons (PAH). Due to the presence of stable benzene rings, most of the PAH show strong inhibition towards biological degradation and the common methods employed for their removal. According to environmental protection agency, most of the PAH are highly toxic in nature. TiO2 photochemistry has been extensively investigated as a method for the catalytic conversion of such organic compounds, highlighting the potential of thereof in the green chemistry. There are actually two methods for the removal of pollutants from the ecosystem. Complete mineralization is the one way to remove pollutants. Conversion of toxic compounds to another compound having toxicity less than the initial starting compound is the second way. Here in this chapter, we are concentrating on the second aspect. The catalysts used were Gd(1wt%)-N-Ti, Pd(1wt%)-N-Ti and Ag(1wt%)-N-Ti. Here we were very successfully converted all the PAH to anthraquinone, a compound having diverse applications in industrial as well as medical fields. Substitution of 10th position of desired PAH by phenyl ring reduces the feasibility of photo reaction and produced 9-hydroxy 9-phenyl anthrone (9H9PA) as an intermediate species. The products were separated and purified by column chromatography using 70:30 hexane/DCM mixtures as the mobile phase and the resultant products were characterized thoroughly by 1H NMR, IR spectroscopy and GCMS analysis. Chapter 6 elucidates the heterogeneous Suzuki coupling reaction by Cu/Pd bimetallic supported on TiO2. Sol-Gel followed by impregnation method was adopted for the synthesis of Cu/Pd-TiO2. The prepared system was characterized by XRD, TG-DTG, SEM, EDX, BET Surface area and XPS. The product was separated and purified by column chromatography using hexane as the mobile phase. Maximum isolated yield of biphenyl of around72% was obtained in DMF using Cu(2wt%)-Pd(4wt%)-Ti as the catalyst. In this reaction, effective solvent, base and catalyst were found to be DMF, K2CO3 and Cu(2wt%)-Pd(4wt%)-Ti respectively. Chapter 7 gives an idea about the photovoltaic (PV) applications of TiO2 based thin films. Due to energy crisis, the whole world is looking for a new sustainable energy source. Harnessing solar energy is one of the most promising ways to tackle this issue. The present dominant photovoltaic (PV) technologies are based on inorganic materials. But the high material, low power conversion efficiency and manufacturing cost limits its popularization. A lot of research has been conducted towards the development of low-cost PV technologies, of which organic photovoltaic (OPV) devices are one of the promising. Here two TiO2 thin films having different thickness were prepared by spin coating technique. The prepared films were characterized by XRD, AFM and conductivity measurements. The thickness of the films was measured by Stylus Profiler. This chapter mainly concentrated on the fabrication of an inverted hetero junction solar cell using conducting polymer MEH-PPV as photo active layer. Here TiO2 was used as the electron transport layer. Thin films of MEH-PPV were also prepared using spin coating technique. Two fullerene derivatives such as PCBM and ICBA were introduced into the device in order to improve the power conversion efficiency. Effective charge transfer between the conducting polymer and ICBA were understood from fluorescence quenching studies. The fabricated Inverted hetero junction exhibited maximum power conversion efficiency of 0.22% with ICBA as the acceptor molecule. Chapter 8 narrates the third order order nonlinear optical properties of bare and noble metal modified TiO2 thin films. Thin films were fabricatedby spray pyrolysis technique. Sol-Gel derived Ti[OCH(CH3)2]4 in CH3CH2OH/CH3COOH was used as the precursor for TiO2. The precursors used for Au, Ag and Pd were the aqueous solutions of HAuCl4, AgNO3 and Pd(NO3)2 respectively. The prepared films were characterized by XRD, SEM and EDX. The nonlinear optical properties of the prepared materials were investigated by Z-Scan technique comprising of Nd-YAG laser (532 nm,7 ns and10 Hz). The non-linear coefficients were obtained by fitting the experimental Z-Scan plot with the theoretical plots. Nonlinear absorption is a phenomenon defined as a nonlinear change (increase or decrease) in absorption with increasing of intensity. This can be mainly divided into two types: saturable absorption (SA) and reverse saturable absorption (RSA). Depending on the pump intensity and on the absorption cross- section at the excitation wavelength, most molecules show non- linear absorption. With increasing intensity, if the excited states show saturation owing to their long lifetimes, the transmission will show SA characteristics. Here absorption decreases with increase of intensity. If, however, the excited state has strong absorption compared with that of the ground state, the transmission will show RSA characteristics. Here in our work most of the materials show SA behavior and some materials exhibited RSA behavior. Both these properties purely depend on the nature of the materials and alignment of energy states within them. Both these SA and RSA have got immense applications in electronic devices. The important results obtained from various studies are presented in chapter 9.

Exploration of Novel Organic Reactions Catalyzed by Nucleophilic Heterocyclic Carbenes (NHCs)

The thesis entitled “Exploration of Novel Organic Reactions Catalyzed by Nucleophilic Heterocyclic Carbenes (NHCs)” embodies the results of the investigations carried out to explore the synthetic potential of N–heterocyclic carbenes (NHCs) as organocatalyst towards various electrophiles for the synthesis of heterocyclic and carbocyclic systems. Recent investigations in the generation of homoenolates by the addition of NHCs to conjugated aldehydes have made it possible to study the reactivity of this unique three carbon synthon.

Design and study of self-assembled functional organic and hybrid systems for biological applications

The focus of self-assembly as a strategy for the synthesis has been confined largely to molecules, because of the importance of manipulating the structure of matter at the molecular scale. We have investigated the influence of temperature and pH, in addition to the concentration of the capping agent used for the formation of the nano-bio conjugates. For example, the formation of the narrower size distribution of the nanoparticles was observed with the increase in the concentration of the protein, which supports the fact that γ-globulin acts both as a controller of nucleation as well as stabiliser. As analyzed through various photophysical, biophysical and microscopic techniques such as TEM, AFM, C-AFM, SEM, DLS, OPM, CD and FTIR, we observed that the initial photoactivation of γ-globulin at pH 12 for 3 h resulted in small protein fibres of ca. Further irradiation for 24 h, led to the formation of selfassembled long fibres of the protein of ca. 5-6 nm and observation of surface plasmon resonance band at around 520 nm with the concomitant quenching of luminescence intensity at 680 nm. The observation of light triggered self-assembly of the protein and its effect on controlling the fate of the anchored nanoparticles can be compared with the naturally occurring process such as photomorphogenesis.Furthermore,our approach offers a way to understand the role played by the self-assembly of the protein in ordering and knock out of the metal nanoparticles and also in the design of nano-biohybrid materials for medicinal and optoelectronic applications. Investigation of the potential applications of NIR absorbing and water soluble squaraine dyes 1-3 for protein labeling and anti-amyloid agents forms the subject matter of the third chapter of the thesis. The study of their interactions with various proteins revealed that 1-3 showed unique interactions towards serum albumins as well as lysozyme. 69%, 71% and 49% in the absorption spectra as well as significant quenching in the fluorescence intensity of the dyes 1-3, respectively. Half-reciprocal analysis of the absorption data and isothermal titration calorimetric (ITC) analysis of the titration experiments gave a 1:1 stoichiometry for the complexes formed between the lysozyme and squaraine dyes with association constants (Kass) in the range 104-105 M-1. We have determined the changes in the free energy (ΔG) for the complex formation and the values are found to be -30.78, -32.31 and -28.58 kJmol-1, respectively for the dyes 1, 2 and 3. Furthermore, we have observed a strong induced CD (ICD) signal corresponding to the squaraine chromophore in the case of the halogenated squaraine dyes 2 and 3 at 636 and 637 nm confirming the complex formation in these cases. To understand the nature of interaction of the squaraine dyes 1-3 with lysozyme, we have investigated the interaction of dyes 1-3 with different amino acids. These results indicated that the dyes 1-3 showed significant interactions with cysteine and glutamic acid which are present in the side chains of lysozyme. In addition the temperature dependent studies have revealed that the interaction of the dye and the lysozyme are irreversible. Furthermore, we have investigated the interactions of these NIR dyes 1-3 with β- amyloid fibres derived from lysozyme to evaluate their potential as inhibitors of this biologically important protein aggregation. These β-amyloid fibrils were insoluble protein aggregates that have been associated with a range of neurodegenerative diseases, including Huntington, Alzheimer’s, Parkinson’s, and Creutzfeldt-Jakob diseases. We have synthesized amyloid fibres from lysozyme through its incubation in acidic solution below pH 4 and by allowing to form amyloid fibres at elevated temperature. To quantify the binding affinities of the squaraine dyes 1-3 with β-amyloids, we have carried out the isothermal titration calorimetric (ITC) measurements. The association constants were determined and are found to be 1.2 × 105, 3.6× 105 and 3.2 × 105 M-1 for the dyes, 1-3, respectively. To gain more insights into the amyloid inhibiting nature of the squaraine dyes under investigations, we have carried out thioflavin assay, CD, isothermal titration calorimetry and microscopic analysis. The addition of the dyes 1-3 (5μM) led to the complete quenching in the apparent thioflavin fluorescence, thereby indicating the destabilization of β-amyloid fibres in the presence of the squaraine dyes. Further, the inhibition of the amyloid fibres by the squaraine dyes 1-3, has been evidenced though the DLS, TEM AFM and SAED, wherein we observed the complete destabilization of the amyloid fibre and transformation of the fibre into spherical particles of ca. These results demonstrate the fact that the squaraine dyes 1-3 can act as protein labeling agents as well as the inhibitors of the protein amyloidogenesis. The last chapter of the thesis describes the synthesis and investigation of selfassembly as well as bio-imaging aspects of a few novel tetraphenylethene conjugates 4-6.Expectedly, these conjugates showed significant solvatochromism and exhibited a hypsochromic shift (negative solvatochromism) as the solvent polarity increased, and these observations were justified though theoretical studies employing the B3LYP/6-31g method. We have investigated the self-assembly properties of these D-A conjugates though variation in the percentage of water in acetonitrile solution due to the formation of nanoaggregates. Further the contour map of the observed fluorescence intensity as a function of the fluorescence excitation and emission wavelength confirmed the formation of J-type aggregates in these cases. To have a better understanding of the type of self-assemblies formed from the TPE conjugates 4-6, we have carried out the morphological analysis through various microscopic techniques such as DLS, SEM and TEM. 70%, we observed rod shape architectures having ~ 780 nm in diameter and ~ 12 μM in length as evidenced through TEM and SEM analysis. We have made similar observations with the dodecyl conjugate 5 at ca. 70% and 50% water/acetonitrile mixtures, the aggregates formed from 4 and 5 were found to be highly crystalline and such structures were transformed to amorphous nature as the water fraction was increased to 99%. To evaluate the potential of the conjugate as bio-imaging agents, we have carried out their in vitro cytotoxicity and cellular uptake studies though MTT assay, flow cytometric and confocal laser scanning microscopic techniques. Thus nanoparticle of these conjugates which exhibited efficient emission, large stoke shift, good stability, biocompatibility and excellent cellular imaging properties can have potential applications for tracking cells as well as in cell-based therapies. In summary we have synthesized novel functional organic chromophores and have studied systematic investigation of self-assembly of these synthetic and biological building blocks under a variety of conditions. The investigation of interaction of water soluble NIR squaraine dyes with lysozyme indicates that these dyes can act as the protein labeling agents and the efficiency of inhibition of β-amyloid indicate, thereby their potential as anti-amyloid agents.

Provenance, Isolation and Characterisation of Organic Matter in the Cochin Estuarine Sediment-“a Diagenetic Amino Acid Marker Scenario

Cochin estuarine system is among the most productive aquatic environment along the Southwest coast of India, exhibits unique ecological features and possess greater socioeconomic relevance. Serious investigations carried out during the past decades on the hydro biogeochemical variables pointed out variations in the health and ecological functioning of this ecosystem. Characterisation of organic matter in the estuary has been attempted in many investigations. But detailed studies covering the degradation state of organic matter using molecular level approach is not attempted. The thesis entitled Provenance, Isolation and Characterisation of Organic Matter in the Cochin Estuarine Sediment-“ A Diagenetic Amino Acid Marker Scenario” is an integrated approach to evaluate the source, quantity, quality, and degradation state of the organic matter in the surface sediments of Cochin estuarine system with the combined application of bulk and molecular level tools. Sediment and water samples from nine stations situated at Cochin estuary were collected in five seasonal sampling campaigns, for the biogeochemical assessment and their distribution pattern of sedimentary organic matter. The sampling seasons were described and abbreviated as follows: April- 2009 (pre monsoon: PRM09), August-2009 (monsoon: MON09), January-2010 (post monsoon: POM09), April-2010 (pre monsoon: PRM10) and September- 2012 (monsoon: MON12). In order to evaluate the general environmental conditions of the estuary, water samples were analysed for water quality parameters, chlorophyll pigments and nutrients by standard methods. Investigations suggested the fact that hydrographical variables and nutrients in Cochin estuary supports diverse species of flora and fauna. Moreover the sedimentary variables such as pH, Eh, texture, TOC, fractions of nitrogen and phosphorous were determined to assess the general geochemical setting as well as redox status. The periodically fluctuating oxic/ anoxic conditions and texture serve as the most significant variables controlling other variables of the aquatic environment. The organic matter in estuary comprise of a complex mixture of autochthonous as well as allochthonous materials. Autochthonous input is limited or enhanced by the nutrient elements like N and P (in their various fractions), used as a tool to evaluate their bioavailability. Bulk parameter approach like biochemical composition, stoichiometric elemental ratios and stable carbon isotope ratio was also employed to assess the quality and quantity of sedimentary organic matter in the study area. Molecular level charactersation of free sugars and amino acids were carried out by liquid chromatographic techniques. Carbohydrates are the products of primary production and their occurrence in sediments as free sugars can provide information on the estuarine productivity. Amino acid biogeochemistry provided implications on the system productivity, nature of organic matter as well as degradation status of the sedimentary organic matter in the study area. The predominance of carbohydrates over protein indicated faster mineralisation of proteinaceous organic matter in sediments and the estuary behaves as a detrital trap for the accumulation of aged organic matter. The higher lipid content and LPD/CHO ratio pointed towards the better food quality that supports benthic fauna and better accumulation of lipid compounds in the sedimentary environment. Allochthonous addition of carbohydrates via terrestrial run off was responsible for the lower PRT/CHO ratio estimated in thesediments and the lower ratios also denoted a detrital heterotrophic environment. Biopolymeric carbon and the algal contribution to BPC provided important information on the better understanding the trophic state of the estuarine system and the higher values of chlorophyll-a to phaeophytin ratio indicated deposition of phytoplankton to sediment at a rapid rate. The estimated TOC/TN ratios implied the combined input of both terrestrial and autochthonous organic matter to sedimentsAmong the free sugars, depleted levels of glucose in sediments in most of the stations and abundance of mannose at station S5 was observed during the present investigation. Among aldohexoses, concentration of galactose was found to be higher in most of the stationsRelative abundance of AAs in the estuarine sediments based on seasons followed the trend: PRM09-Leucine > Phenylalanine > Argine > Lysine, MON09-Lysine > Aspartic acid > Histidine > Tyrosine > Phenylalanine, POM09-Lysine > Histadine > Phenyalanine > Leucine > Methionine > Serine > Proline > Aspartic acid, PRM10-Valine > Aspartic acid > Histidine > Phenylalanine > Serine > Proline, MON12-Lysine > Phenylalanine > Aspartic acid > Histidine > Valine > Tyrsine > MethionineThe classification of study area into three zones based on salinity was employed in the present study for the sake of simplicity and generalized interpretations. The distribution of AAs in the three zones followed the trend: Fresh water zone (S1, S2):- Phenylalanine > Lysine > Aspartic acid > Methionine > Valine ῀ Leucine > Proline > Histidine > Glycine > Serine > Glutamic acid > Tyrosine > Arginine > Alanine > Threonine > Cysteine > Isoleucine. Estuarine zone (S3, S4, S5, S6):- Lysine > Aspartic acid > Phenylalanine > Leucine > Valine > Histidine > Methionine > Tyrosine > Serine > Glutamic acid > Proline > Glycine > Arginine > Alanine > Isoleucine > Cysteine > Threonine. Riverine /Industrial zone (S7, S8, S9):- Phenylalanine > Lysine > Aspartic acid > Histidine > Serine > Arginine > Tyrosine > Leucine > Methionine > Glutamic acid > Alanine > Glycine > Cysteine > Proline > Isoleucine > Threonine > Valine. The abundance of AAs like glutamic acid, aspartic acid, isoleucine, valine, tyrosine, and phenylalanine in sediments of the study area indicated freshly derived organic matter.

A Study of Single Stage Semi‐Dry Anaerobic Digestion of Organic Fraction of Municipal Solid Waste

Solid waste generation is a natural consequence of human activity and is increasing along with population growth, urbanization and industrialization. Improper disposal of the huge amount of solid waste seriously affects the environment and contributes to climate change by the release of greenhouse gases. Practicing anaerobic digestion (AD) for the organic fraction of municipal solid waste (OFMSW) can reduce emissions to environment and thereby alleviate the environmental problems together with production of biogas, an energy source, and digestate, a soil amendment. The amenability of substrate for biogasification varies from substrate to substrate and different environmental and operating conditions such as pH, temperature, type and quality of substrate, mixing, retention time etc. Therefore, the purpose of this research work is to develop feasible semi-dry anaerobic digestion process for the treatment of OFMSW from Kerala, India for potential energy recovery and sustainable waste management. This study was carried out in three phases in order to reach the research purpose. In the first phase, batch study of anaerobic digestion of OFMSW was carried out for 100 days at 32°C (mesophilic digestion) for varying substrate concentrations. The aim of this study was to obtain the optimal conditions for biogas production using response surface methodology (RSM). The parameters studied were initial pH, substrate concentration and total organic carbon (TOC). The experimental results showed that the linear model terms of initial pH and substrate concentration and the quadratic model terms of the substrate concentration and TOC had significant individual effect (p < 0.05) on biogas yield. However, there was no interactive effect between these variables (p > 0.05). The optimum conditions for maximizing the biogas yield were a substrate concentration of 99 g/l, an initial pH of 6.5 and TOC of 20.32 g/l. AD of OFMSW with optimized substrate concentration of 99 g/l [Total Solid (TS)-10.5%] is a semi-dry digestion system .Under the optimized condition, the maximum biogas yield was 53.4 L/kg VS (volatile solid).. In the second phase, semi-dry anaerobic digestion of organic solid wastes was conducted for 45 days in a lab-scale batch experiment for substrate concentration of 100 g/l (TS-11.2%) for investigating the start-up performances under thermophilic condition (50°C). The performance of the reactor was evaluated by measuring the daily biogas production and calculating the degradation of total solids and the total volatile solids. The biogas yield at the end of the digestion was 52.9 L/kg VS for the substrate concentration of 100 g/l. About 66.7% of volatile solid degradation was obtained during the digestion. A first order model based on the availability of substrate as the limiting factor was used to perform the kinetic studies of batch anaerobic digestion system. The value of reaction rate constant, k, obtained was 0.0249 day-1. A laboratory bench scale reactor with a capacity of 36.8 litres was designed and fabricated to carry out the continuous anaerobic digestion of OFMSW in the third phase. The purpose of this study was to evaluate the performance of the digester at total solid concentration of 12% (semi-dry) under mesophlic condition (32°C). The digester was operated with different organic loading rates (OLRs) and constant retention time. The performance of the reactor was evaluated using parameters such as pH, volatile fatty acid (VFA), alkalinity, chemical oxygen demand (COD), TOC and ammonia-N as well as biogas yield. During the reactor’s start-up period, the process is stable and there is no inhibition occurred and the average biogas production was 14.7 L/day. The reactor was fed in continuous mode with different OLRs (3.1,4.2 and 5.65 kg VS/m3/d) at constant retention time of 30 days. The highest volatile solid degradation of 65.9%, with specific biogas production of 368 L/kg VS fed was achieved with OLR of 3.1 kg VS/m3/d. Modelling and simulation of anaerobic digestion of OFMSW in continuous operation is done using adapted Anaerobic Digestion Model No 1 (ADM1).The proposed model, which has 34 dynamic state variables, considers both biochemical and physicochemical processes and contains several inhibition factors including three gas components. The number of processes considered is 28. The model is implemented in Matlab® version 7.11.0.584(R2010b). The model based on adapted ADM1 was tested to simulate the behaviour of a bioreactor for the mesophilic anaerobic digestion of OFMSW at OLR of 3.1 kg VS/m3/d. ADM1 showed acceptable simulating results.

Organic field-effect transistors and phototransistors based on amorphous materials

A comparison between the charge transport properties in low molecular amorphous thin films of spiro-linked compound and their corresponding parent compound has been demonstrated. The field-effect transistor method is used for extracting physical parameters such as field-effect mobility of charge carriers, ON/OFF ratios, and stability. In addition, phototransistors have been fabricated and demonstrated for the first time by using organic materials. In this case, asymmetrically spiro-linked compounds are used as active materials. The active materials used in this study can be divided into three classes, namely Spiro-linked compounds (symmetrically spiro-linked compounds), the corresponding parent-compounds, and photosensitive spiro-linked compounds (asymmetrically spiro-linked com-pounds). Some of symmetrically spiro-linked compounds used in this study were 2,2',7,7'-Tetrakis-(di-phenylamino)-9,9'-spirobifluorene (Spiro-TAD),2,2',7,7'-Tetrakis-(N,N'-di-p-methylphenylamino)-9,9'-spirobifluorene (Spiro-TTB), 2,2',7,7'-Tetra-(m-tolyl-phenylamino)-9,9'-spirobifluorene (Spiro-TPD), and 2,2Ž,7,7Ž-Tetra-(N-phenyl-1-naphtylamine)-9,9Ž-spirobifluorene (Spiro alpha-NPB). Related parent compounds of the symmetrically spiro-linked compound used in this study were N,N,N',N'-Tetraphenylbenzidine (TAD), N,N,N',N'-Tetrakis(4-methylphenyl)benzidine (TTB), N,N'-Bis(3-methylphenyl)-(1,1'-biphenyl)-4,4'-diamine (TPD), and N,N'-Diphenyl-N,N'-bis(1-naphthyl)-1,1'-biphenyl-4,4'-diamine (alpha-NPB). The photosensitive asymmetrically spiro-linked compounds used in this study were 2,7-bis-(N,N'-diphenylamino)-2',7'-bis(biphenyl-4-yl)-9,9'-spirobifluorene (Spiro-DPSP), and 2,7-bis-(N,N'-diphenylamino)-2',7'-bis(spirobifluorene-2-yl)-9,9'-spirobifluorene (Spiro-DPSP^2). It was found that the field-effect mobilities of charge carriers in thin films of symmetrically spiro-linked compounds and their corresponding parent compounds are in the same order of magnitude (~10^-5 cm^2/Vs). However, the thin films of the parent compounds were easily crystallized after the samples have been exposed in ambient atmosphere and at room temperature for three days. In contrast, the thin films and the transistor characteristics of symmetrically spiro-linked compound did not change significantly after the samples have been stored in ambient atmosphere and at room temperature for several months. Furthermore, temperature dependence of the mobility was analyzed in two models, namely the Arrhenius model and the Gaussian Disorder model. The Arrhenius model tends to give a high value of the prefactor mobility. However, it is difficult to distinguish whether the temperature behaviors of the material under consideration follows the Arrhenius model or the Gaussian Disorder model due to the narrow accessible range of the temperatures. For the first time, phototransistors have been fabricated and demonstrated by using organic materials. In this case, asymmetrically spiro-linked compounds are used as active materials. Intramolecular charge transfer between a bis(diphenylamino)biphenyl unit and a sexiphenyl unit leads to an increase in charge carrier density, providing the amplification effect. The operational responsivity of better than 1 A/W can be obtained for ultraviolet light at 370 nm, making the device interesting for sensor applications. This result offers a new potential application of organic thin film phototransistors as low-light level and low-cost visible blind ultraviolet photodetectors.

Microbial use of organic substrates and maize growth, especially in saline and alkaline soils of Pakistani Punjab

This thesis consists of 4 main parts: (1) impact of growing maize on the decomposition of incorporated fresh alfalfa residues, (2) relationships between soil biological and other soil properties in saline and alkaline arable soils from the Pakistani Punjab, (3) decomposition of compost and plant residues in Pakistani soils along a gradient in salinity, and (4) interactions of compost and triple superphosphate on the growth of maize in a saline Pakistani soil. These 4 chapters are framed by a General Introduction and a Conclusions section. (1) In the first study, the effects of growing maize plants on the microbial decomposition of freshly chopped alfalfa residues was investigated in a 90-day pot experiment using a sandy arable soil. Assuming that the addition of alfalfa residues did not affect the decomposition of native soil organic matter, only 27% of the alfalfa residues were found as CO2. This suggests that a considerable part of alfalfa-C remained undecomposed in the soil. However, only 6% of the alfalfa residues could be recovered as plant remains in treatment with solely alfalfa residues. Based on d13C values, it was calculated that plant remains in treatment maize + alfalfa residues contained 14.7% alfalfa residues and 85.3% maize root remains. This means 60% more alfalfa-C was recovered in this treatment. (2) In the second study, the interactions between soil physical, soil chemical and soil biological properties were analysed in 30 Pakistani soils from alkaline and saline arable sites differing strongly in salinisation and in soil pH. The soil biological properties were differentiated into indices for microbial activity, microbial biomass, and community structure with the aim of assessing their potential as soil fertility indices. (3) In the third study, 3 organic amendments (compost, maize straw and pea straw) were added to 5 Pakistani soils from a gradient in salinity. Although salinity has depressive effects on microbial biomass C, biomass N, biomass P, and ergosterol, the clear gradient according to the soil salt concentration was not reflected by the soil microbial properties. The addition of the 3 organic amendments always increased the contents of the microbial indices analysed. The amendment-induced increase was especially strong for microbial biomass P and reflected the total P content of the added substrates. (4) The fourth study was greenhouse pot experiment with different combinations of compost and triple superphosphate amendments to investigate the interactions between plant growth, microbial biomass formation and compost decomposition in a strongly saline Pakistani arable soil in comparison to a non-saline German arable soil. The Pakistani soil had a 2 times lower content of ergosterol, a 4 times lower contents of microbial biomass C, biomass N and biomass P, but nearly a 20 times lower content of NaHCO3 extractable P. The addition of 1% compost always had positive effects on the microbial properties and also on the content of NaHCO3 extractable P. The addition of superphosphate induced a strong and similar absolute increase in microbial biomass P in both soils.

Soil organic carbon management for sustainable land use in Sudano-Sahelian West Africa

Judged by their negative nutrient balances, low soil cover and low productivity, the predominant agro-pastoral farming systems in the Sudano-Sahelian zone of West Africa are highly unsustainable for crop production intensification. With kaolinite as the main clay type, the cation exchange capacity of the soils in this region, often less than 1 cmol_c kg^-1 soil, depends heavily on the organic carbon (Corg) content. However, due to low carbon sequestration and to the microbe, termite and temperature-induced rapid turnover rates of organic material in the present land-use systems, Corg contents of the topsoil are very low, ranging between 1 and 8 g kg^-1 in most soils. For sustainable food production, the availability of phosphorus (P) and nitrogen (N) has to be increased considerably in combination with an improvement in soil physical properties. Therefore, the adoption of innovative management options that help to stop or even reverse the decline in Corg typically observed after cultivating bush or rangeland is of utmost importance. To maintain food production for a rapidly growing population, targeted applications of mineral fertilisers and the effective recycling of organic amendments as crop residues and manure are essential. Any increase in soil cover has large effects in reducing topsoil erosion by wind and water and favours the accumulation of wind-blown dust high in bases which in turn improves P availability. In the future decision support systems, based on GIS, modelling and simulation should be used to combine (i) available fertiliser response data from on-station and on-farm research, (ii) results on soil productivity restoration with the application of mineral and organic amendments and (iii) our present understanding of the cause-effect relationships governing the prevailing soil degradation processes. This will help to predict the effectiveness of regionally differentiated soil fertility management approaches to maintain or even increase soil Corg levels.

Composition and stability of organic matter fractions in soils under different land use regimes

Soil organic matter (SOM) vitally impacts all soil functions and plays a key role in the global carbon (C) cycle. More than 70% of the terrestric C stocks that participate in the active C cycle are stored in the soil. Therefore, quantitative knowledge of the rates of C incorporation into SOM fractions of different residence time is crucial to understand and predict the sequestration and stabilization of soil organic carbon (SOC). Consequently, there is a need of fractionation procedures that are capable of isolating functionally SOM fractions, i.e. fractions that are defined by their stability. The literature generally refers to three main mechanisms of SOM stabilization: protection of SOM from decomposition by (i) its structural composition, i.e. recalcitrance, (ii) spatial inaccessibility and/or (iii) interaction with soil minerals and metal ions. One of the difficulties in developing fractionation procedures for the isolation of functional SOM fractions is the marked heterogeneity of the soil environment with its various stabilization mechanisms – often several mechanisms operating simultaneously – in soils and soil horizons of different texture and mineralogy. The overall objective of the present thesis was to evaluate present fractionation techniques and to get a better understanding of the factors of SOM sequestration and stabilization. The first part of this study is attended to the structural composition of SOM. Using 13C cross-polarization magic-angle spinning (CPMAS) nuclear magnetic resonance (NMR) spectroscopy, (i) the effect of land use on SOM composition was investigated and (ii) examined whether SOM composition contributes to the different stability of SOM in density and aggregate fractions. The second part of the present work deals with the mineral-associated SOM fraction. The aim was (iii) to evaluate the suitability of chemical fractionation procedures used in the literature for the isolation of stable SOM pools (stepwise hydrolysis, treatments using oxidizing agents like Na2S2O8, H2O2, and NaOCl as well as demineralization of the residue obtained by the NaOCl treatment using HF (NaOCl+HF)) by pool sizes, 13C and 14C data. Further, (iv) the isolated SOM fractions were compared to the inert organic matter (IOM) pool obtained for the investigated soils using the Rothamsted Carbon Model and isotope data in order to see whether the tested chemical fractionation methods produce SOM fractions capable to represent this pool. Besides chemical fractionation, (v) the suitability of thermal oxidation at different temperatures for obtaining stable SOC pools was evaluated. Finally, (vi) the short-term aggregate dynamics and the factors that impact macroaggregate formation and C stabilization were investigated by means of an incubation study using treatments with and without application of 15N labeled maize straw of different degradability (leaves and coarse roots). All treatments were conducted with and without the addition of fungicide. Two study sites with different soil properties and land managements were chosen for these investigations. The first one, located at Rotthalmünster, is a Stagnic Luvisol (silty loam) under different land use regimes. The Ah horizons of a spruce forest and continuous grassland and the Ap and E horizons of two plots with arable crops (continuous maize and wheat cropping) were examined. The soil of the second study site, located at Halle, is a Haplic Phaeozem (loamy sand) where the Ap horizons of two plots with arable crops (continuous maize and rye cropping) were investigated. Both study sites had a C3-/C4-vegetational change on the maize plot for the purpose of tracing the incorporation of the younger, maize-derived C into different SOM fractions and the calculation of apparent C turnover times of these. The Halle site is located near a train station and industrial areas, which caused a contamination with high amounts of fossil C. The investigation of aggregate and density fractions by 13C CPMAS NMR spectroscopy revealed that density fractionation isolated SOM fractions of different composition. The consumption of a considerable part (10–20%) of the easily available O-alkyl-C and the selective preservation of the more recalcitrant alkyl-C when passing from litter to the different particulate organic matter (POM) fractions suggest that density fractionation was able to isolate SOM fractions with different degrees of decomposition. The spectra of the aggregate fractions resembled those of the mineral-associated SOM fraction obtained by density fractionation and no considerable differences were observed between aggregate size classes. Comparison of plant litter, density and aggregate size fractions from soil under different land use showed that the type of land use markedly influenced the composition of SOM. While SOM of the acid forest soil was characterized by a large content (> 50%) of POM, which contained high amounts of spruce-litter derived alkyl-C, the organic matter in the biologically more active grassland and arable soils was dominated by mineral-associated SOM (> 95%). This SOM fraction comprised greater proportions of aryl- and carbonyl-C and is considered to contain a higher amount of microbially-derived organic substances. Land use can alter both, structure and stability of SOM fractions. All applied chemical treatments induced considerable SOC losses (> 70–95% of mineral-associated SOM) in the investigated soils. The proportion of residual C after chemical fractionation was largest in the arable Ap and E horizons and increased with decreasing C content in the initial SOC after stepwise hydrolysis as well as after the oxidative treatments with H2O2 and Na2S2O8. This can be expected for a functional stable pool of SOM, because it is assumed that the more easily available part of SOC is consumed first if C inputs decrease. All chemical treatments led to a preferential loss of the younger, maize-derived SOC, but this was most pronounced after the treatments with Na2S2O8 and H2O2. After all chemical fractionations, the mean 14C ages of SOC were higher than in the mineral-associated SOM fraction for both study sites and increased in the order: NaOCl < NaOCl+HF ≤ stepwise hydrolysis << H2O2 ≈ Na2S2O8. The results suggest that all treatments were capable of isolating a more stable SOM fraction, but the treatments with H2O2 and Na2S2O8 were the most efficient ones. However, none of the chemical fractionation methods was able to fit the IOM pool calculated using the Rothamsted Carbon Model and isotope data. In the evaluation of thermal oxidation for obtaining stable C fractions, SOC losses increased with temperature from 24–48% (200°C) to 100% (500°C). In the Halle maize Ap horizon, losses of the young, maize-derived C were considerably higher than losses of the older C3-derived C, leading to an increase in the apparent C turnover time from 220 years in mineral-associated SOC to 1158 years after thermal oxidation at 300°C. Most likely, the preferential loss of maize-derived C in the Halle soil was caused by the presence of the high amounts of fossil C mentioned above, which make up a relatively large thermally stable C3-C pool in this soil. This agrees with lower overall SOC losses for the Halle Ap horizon compared to the Rotthalmünster Ap horizon. In the Rotthalmünster soil only slightly more maize-derived than C3-derived SOC was removed by thermal oxidation. Apparent C turnover times increased slightly from 58 years in mineral-associated SOC to 77 years after thermal oxidation at 300°C in the Rotthalmünster Ap and from 151 to 247 years in the Rotthalmünster E horizon. This led to the conclusion that thermal oxidation of SOM was not capable of isolating SOM fractions of considerably higher stability. The incubation experiment showed that macroaggregates develop rapidly after the addition of easily available plant residues. Within the first four weeks of incubation, the maximum aggregation was reached in all treatments without addition of fungicide. The formation of water-stable macroaggregates was related to the size of the microbial biomass pool and its activity. Furthermore, fungi were found to be crucial for the development of soil macroaggregates as the formation of water-stable macroaggregates was significantly delayed in the fungicide treated soils. The C concentration in the obtained aggregate fractions decreased with decreasing aggregate size class, which is in line with the aggregate hierarchy postulated by several authors for soils with SOM as the major binding agent. Macroaggregation involved incorporation of large amounts maize-derived organic matter, but macroaggregates did not play the most important role in the stabilization of maize-derived SOM, because of their relatively low amount (less than 10% of the soil mass). Furthermore, the maize-derived organic matter was quickly incorporated into all aggregate size classes. The microaggregate fraction stored the largest quantities of maize-derived C and N – up to 70% of the residual maize-C and -N were stored in this fraction.

Organic inputs and farmers' management strategies in millet fields of western Niger

Research on soil fertility management in sub-Saharan Africa was criticized lately for largely ignoring farmers’ management strategies and the underlying principles. To fill this gap of knowledge, detailed interviews were conducted with 108 farm households about their rationale in managing the soil fertility of 307 individual fields in the agro-pastoral village territory of Chikal in western Niger. To amplify the farmers’ information on manuring and corralling practices, repeated measurements of applied amounts of manure were carried out within six 1-km^2 monitoring areas from February to October 1998. The interviews revealed that only 2% of the fields were completely fallowed for a period of 1–15 years, but 40% of the fields were at least partially fallowed. Mulching of crop residues was mainly practiced to fight wind erosion but was restricted to 36% of the surveyed fields given the alternative use of straw as livestock feed. Manure application and livestock corralling, as most effective tools to enhance soil fertility, were targeted to less than 30% of the surveyed fields. The application of complete fallow and manuring and corralling practices were strongly related to the households’ endowment with resources, especially with land and livestock. Within particular fields, measures were mainly applied to spots of poor soil fertility, while the restoration of the productivity of hard pans was of secondary importance. Given the limited spatial coverage of indigenous soil fertility measures and their strong dependence on farmers’ wealth, supplementary strategies to restrict the decline of soil fertility in the drought prone areas of Niger with their heavily weathered soils are needed.

Organic potatoes for processing

Drei Feldversuche auf zwei Standorten (DFH: 51°4, 9°4’, BEL: 52°2’, 8°08’) wurden in den Jahren 2002 bis 2004 durchgeführt, um den Einfluss der Vorfrucht, des Vorkeimens, der N- und K-Düngung und der Sorte auf Nährstoffverfügbarkeit, Gesamt- und sortierte Knollenerträge sowie die Qualität von Kartoffeln und deren Eignung für die industrielle Verarbeitung zu Pommes frites und Chips zu untersuchen. Bestimmt wurden die N- und K-Verfügbarkeit im Boden, die N- und K-Aufnahme von Kraut und Knollen, gesamte Frisch- und Trockenmasseerträge, sortierte Frischmasseerträge für die Verarbeitung, sowie die Gehalte der Knollen an Trockensubstanz und reduzierenden Zuckern. In einer sensorischen Prüfung wurden Qualitätsparameter von Pommes frites (Aussehen/Farbe, Textur und Geschmack/Geruch) bewertet, die gewichtet in einen Qualitätsindex eingingen. Die Qualität der Chips wurde maschinell durch den L-Wert (Helligkeit) des Produktes quantifiziert. Der Gehalt des Bodens an mineralisiertem Nitrat-Stickstoff hing von der Vorfrucht und dem Jahr ab. Nach Erbsen wurden zum Auflaufen der Kartoffeln in den Versuchsjahren 2003 und 2004 (187 und 132 kg NO3-N ha-1) die höchsten NO3-N-Werte in 0-60 cm Boden gemessen verglichen mit Kleegras (169 bzw. 108 kg NO3-N ha-1 oder Getreide (112 kg bzw. 97 kg NO3-N ha-1), obgleich die Differenz nicht in allen Fällen signifikant war. Entsprechend wurden nach Erbsen die höchsten Knollen-Frischmasseerträge (414 und 308 dt ha-1) geerntet. Dasselbe galt für die Trockenmasserträge, was belegt, dass der Trockensubstanzgehalt der Knollen bei verbesserter N-Versorgung nicht im selben Maße sinkt, wie der Frischmasseertrag steigt. Das Vorkeimen der Pflanzknollen führte zu einer rascheren phänologischen Entwicklung im Jugendstadium der Pflanze, beschleunigter Trockenmassebildung des Krautes und einer früheren Einlagerung von Assimilaten vom Kraut in die Knollen. Obwohl die positive Wirkung des Vorkeimens auf den Gesamtertrag bis Ende Juli (+ 26 in 2003 bzw. 34 dt ha-1 in 2004) im Jahr ohne Krautfäuleepidemie von den nicht vorgekeimten Varianten bis zur Endernte im September kompensiert wurde, konnte in diesem Jahr durch Vorkeimen dennoch ein erhöhter Ertragsanteil (+ 12%) der besonders nachgefragten Übergrößen (>50 mm für Pommes frites) erzielt werden. Die durchschnittliche Knollenmasse reagierte positiv auf Vorkeimen (+ 5,4 g), Sortenwahl (Sorte Agria) und ein erhöhtes N-Angebot (Leguminosenvorfrucht). Generell wurde deutlich, dass die Knollengesamterträge unter den Bedingungen des Ökologischen Landbaus (geringe bis mittlere Nährstoffversorgung, verkürzte Vegetationsdauer) sehr stark vom Anbaujahr abhängen. Die Ergebnisse belegen jedoch, dass organisch-mineralische N-K-Düngung den sortierten Ertrag an Knollen für die Verarbeitung signifikant erhöht: Höchste Gesamt- und sortierte Knollenfrischmasseerträge wurden nach kombinierter N (Horngrieß) und mineralischer K- (Kaliumsulfat) Gabe erzielt (348 dt ha-1 im Durchschnitt von 2002-2004). Im Gegensatz dazu kann eine Wirkung von Stallmist auf den Ertrag im Jahr der Ausbringung nicht unbedingt erwartet werden. Steigende Erträge nach Stallmistdüngung wurden lediglich in einem von drei Versuchsjahren (+58 dt ha-1) festgestellt und ließen sich eher auf eine K- als eine N-Wirkung zurückführen. Die Ergebnisse belegen, dass die Sortenwahl eine entscheidende Rolle spielt, wenn die Kartoffeln für die industrielle Verarbeitung zu den oben genannten Produkten angebaut werden. Insgesamt kann festgestellt werden, dass Kartoffelknollen aus ökologischen Anbauverfahren ausreichend hohe Trockensubstanzgehalte aufweisen, um für die Verarbeitung zu Pommes frites (>19%) geeignet zu sein und ohne dass dadurch die Konsistenz des Endproduktes gefährdet würde. Der Trockensubstanzgehalt der Referenzsorte für Chips, „Marlen“, unterschritt das in der Literatur geforderte Minimum für Chips von 23% lediglich, wenn die kombinierte Horngrieß-Kaliumsulfatdüngung zur Anwendung kam. Die Trockensubstanzgehalte der Knollen konnten durch Vorkeimen signifikant gesteigert werden und der Effekt war besonders groß (+1.2% absolut) in dem Jahr mit frühem Auftreten der Krautfäule (Phytophthora infestans), d.h. verkürzter Vegetationszeit. Die Knollen-Trockensubstanzgehalte waren in zwei von drei Experimenten nach Lagerung höher (+0.4 und 0.5% absolut) als noch zur Ernte. Sorten der sehr frühen und frühen Reifegruppe wiesen den größten relativen Anstieg der Gehalte an reduzierenden Zuckern (Glukose und Fruktose) während der Lagerung auf. Den mittelfrühen Sorten „Agria“ und „Marena“ hingegen kann aufgrund des von ihnen erreichten höchsten Qualitätsstandards (Pommes frites) zur Ernte eine sehr gute Eignung für die Bedingungen des Ökologischen Landbaus unterstellt werden. Die durchgehend beste Chipseignung wies die mittelfrühe Referenzsorte „Marlen“ auf. Insgesamt konnte nachgewiesen werden, dass durch gezielte Sortenwahl der Trockensubstanzgehalt und die Konzentration reduzierender Zucker, sowie die Qualität der Endprodukte (Pommes frites und Chips) gezielt beeinflusst werden kann. Im Gegensatz dazu haben acker- und pflanzenbauliche Maßnahmen wie Düngung, Wahl der Vorfrucht und Vorkeimen der Pflanzknollen einen eher geringen Einfluss. Dementsprechend sollte der Landwirt versuchen, durch die Wahl der Sorte den hohen Anforderungen der Industrie an die Rohware gerecht zu werden.

Einfluß der Gewässerversauerung auf Hyporheos und Bryorheos: Untersuchungen an zwei Waldbächen im Westharz

Im Rahmen der Fallstudie Harz sollte an der Schnittstelle zwischen Grundlagenforschung und angewandter Forschung ein Beitrag zur Klärung der Frage geleistet werden, inwieweit zwei Zuläufe der Sösetalsperre im Westharz versauert bzw. versauerungsgefährdet sind; aus diesem Stausee wird Trinkwasser für mehrere Gemeinden in Norddeutschland gewonnen. Die Belastung des fast vollständig bewaldeten Einzugsgebiets der Sösetalsperre mit luftbürtigen Schadstoffen (Saurer Regen) zählte zu den höchsten in Mitteleuropa. An jeweils drei Untersuchungsstellen der beiden Bäche Alte Riefensbeek (R1 bis R3) und Große Söse (S1 bis S3) wurden zwischen März 1987 und November 1988 Proben aus Moospolstern und dem hyporheischen Interstitial entnommen und physikalisch, chemisch und biologisch untersucht. Ergänzend wurden Wasserproben zwischen März 1986 und Oktober 1991 sowie vom April 1998 ebenso wie qualitative Fänge von Makroinvertebraten zwischen November 1986 und Juli 1990 sowie vom April 1998 ausgewertet. Die Analyse der tierischen Besiedlung der Moos- und Interstitialproben beschränkte sich auf die taxonomischen Gruppen Turbellaria (Strudelwürmer), Mollusca (Weichtiere), Amphipoda (Flohkrebse), Ephemeroptera (Eintagsfliegen), Plecoptera (Steinfliegen), Heteroptera (Wanzen), Megaloptera (Schlammfliegen), Coleoptera (Käfer), Trichoptera (Köcherfliegen) und Diptera (Zweiflügler). Der Grundsatz, daß normalverteilte und nicht normalverteilte Daten statistisch unterschiedlich behandelt werden müssen, wurde konsequent angewandt. Am Beispiel der Choriotopstruktur wurde gezeigt, daß die Auswahl des Analyseverfahrens das Ergebnis der ökologischen Interpretation multivariater statistischer Auswertung beeinflußt. Die Daten der Korngrößen-Verteilung wurden vergleichend einer univariaten und einer multivariaten statistischen Analyse unterworfen. Mit dem univariaten Verfahren wurden die Gradienten der ökologisch relevanten Korngrößen-Parameter eher erkannt als mit dem multivariaten Verfahren. Die Auswirkungen von Gewässerversauerung sowie anderer Umweltfaktoren (insgesamt 42 Faktoren) auf die Lebensgemeinschaften wurden anhand der Parameter Artenzahl, Besiedlungsdichte, Körpergröße und Biomasse untersucht. Abundanz, Biomasse und Körpergröße sowie die Umweltfaktoren wurden auf einem horizontalen Gradienten, d.h. im Längslauf der Bäche, und auf einem vertikalen Gradienten, d.h. fließende Welle / Bryorheon / Benthon versus Hyporheon, untersucht. Es wurde ein terminologisches System für die Kompartimente in der Fließgewässer-Aue vorgeschlagen, das in sich einheitlich ist. Es wurde ein neuer Moos-Vitalitätsindex für die Moospolster vorgestellt. Es wurden Bestimmungsschlüssel für die Larven der Chloroperlidae (Steinfliegen-Familie) und der Empididae (Tanzfliegen) in den beiden Harzbächen entwickelt. Die untersuchten Bachstrecken waren frei von Abwasserbelastung. An zwei Stellen wurde Wasser für einen Forellenteich ausgeleitet. Abgesehen von zwei meterhohen Abstürzen in der Großen Söse waren wasserbauliche Veränderungen ohne große Bedeutung. Das Abfluß-Regime war insofern nicht mehr natürlich, als beide Bäche in das System der bergbaulichen Bewässerungsgräben des Oberharzes eingebunden sind. Die Söse hatte ein F-nivopluviales Abfluß-Regime, der abflußreichste Doppelmonat war der März / April, die Unregelmäßigkeit des Abfluß-Regimes war sehr hoch, die Vorhersagbarkeit sehr niedrig, die monatlichen Abfluß-Maxima wiesen eine sehr geringe Konstanz auf. Der Zeitraum der biologischen Probenahme wurde von überdurchschnittlich vielen Tagen mit mäßig erhöhten Abflüssen geprägt, sehr große Hochwasser-Wellen fehlten aber. Die Abfluß-Dynamik wurde statistisch beschrieben. Das hydraulische Regime wurde anhand der Meßgrößen Fließgeschwindigkeit, Fließkraft und FROUDE-Zahl dargestellt. Der Zusammenhang zwischen Abfluß und Fließgeschwindigkeit auf der einen Seite und der Korngrößen-Verteilung auf der anderen Seite wurde statistisch untersucht, ebenfalls zwischen dem Abfluß und dem Kohlenstoff- und Stickstoff-Gehalt der Feinstpartikel sowie dem Wasserchemismus. In den Phasen ohne Hochwasser hatte das Hyporheal die Funktion einer Senke für Feinstkörner. Das Bachbett der Alten Riefensbeek war stabiler als das der Großen Söse. Insgesamt gesehen war das hyporheische Sediment in den quellnahen Abschnitten grobkörniger und auf den quellfernen Strecken feinkörniger. Der prozentuale Anteil der Feinstkörner im Hyporheal und Benthal nahm aber im Längslauf der Bäche ab. Dies ist ungewöhnlich, konnte aber nicht plausibel mit geologischen und hydrologischen Meßgrößen erklärt werden. Beide Bäche waren sommerkalt. Der Einfluß der Wassertemperatur auf die Larvalentwicklung wurde beispielhaft an den Taxa Baetis spp. und Leuctra gr. inermis untersucht. Es gab eine Tendenz, daß der Kohlenstoff- und Stickstoff-Gehalt der Feinstpartikel vom Benthal in das Hyporheal anstieg. Dies war ein weiterer Hinweis darauf, daß das Hyporheal die Funktion einer Senke und Vorratskammer für Nährstoffe hat. Der Zusammenhang zwischen partikulärer und gelöster Kohlenstoff-Fraktion wurde diskutiert. Im Hyporheon war die Nitrifikation nicht stärker als in der fließenden Welle. Es gab Hinweise, daß die sauren pH-Werte in der Großen Söse die Nitrifikation hemmten. Die Valenzen der Moos- und Tier-Taxa bezüglich Fließgeschwindigkeit, pH-Wert, Alkalinität sowie der Gehalte von Sauerstoff, Calcium, Magnesium, Kalium und Natrium wurden zusammengestellt. Das hyporheische Sediment war sehr grob und hatte eine hohe Porosität. Der Austausch zwischen fließender Welle und hyporheischem Wasser konnte deshalb sehr schnell erfolgen, es gab keine intergranulare Sprungschicht, die physikalischen und chemischen Tiefengradienten waren in den meisten Fällen gar nicht ausgeprägt oder nur sehr flach. Die Wassertemperatur des Freiwassers unterschied sich nicht signifikant von derjenigen im hyporheischen Wasser. Es gab -- von wenigen Ausnahmen bei pH-Wert, Leitfähigkeit und Sauerstoffgehalt abgesehen -- keine signifikanten Unterschiede zwischen dem Wasserchemismus der fließenden Welle und dem des Hyporheals. Die physikalischen und chemischen Voraussetzungen für die Refugialfunktion des Hyporheons waren deshalb für versauerungsempfindliche Taxa nicht gegeben. In der Tiefenverteilung der untersuchten Tiergruppen im Hyporheal lag das Maximum der Abundanz bzw. Biomasse häufiger in 10 cm als in 30 cm Tiefe. Daraus läßt sich aber keine allgemeine Gesetzmäßigkeit ableiten. Es wurde durchgehend die Definition angewendet, daß die Gewässerversauerung durch den Verlust an Pufferkapazität charakterisiert ist. Saure Gewässer können, müssen aber nicht versauert sein; versauerte Gewässer können, müssen aber nicht saures Wasser haben. Maßstab für das Pufferungsvermögen eines Gewässers ist nicht der pH-Wert, sondern sind die Alkalinität und andere chemische Versauerungsparameter. Der pH-Wert war auch operativ nicht als Indikator für Gewässerversauerung anwendbar. Die chemische Qualität des Bachwassers der Großen Söse entsprach aufgrund der Versauerung nicht den umweltrechtlichen Vorgaben bezüglich der Parameter pH-Wert, Aluminium, Eisen und Mangan, bzgl. Zink galt dies nur an S1. In der Alten Riefensbeek genügte das Hyporheal-Wasser in 30 cm Tiefe an R2 bzgl. des Sauerstoff-Gehalts nicht den umweltrechtlichen Anforderungen. Nur im Freiwasser an R1 genügten die Ammonium-Werte den Vorgaben der EG-Fischgewässer-Richtlinie, der Grenzwert wurde an allen anderen Meßstellen und Entnahmetiefen überschritten. Das BSB-Regime in allen Entnahmetiefen an R2, im Freiwasser an R3 und S1, im Hyporheal an R1 sowie in 30 cm Tiefe an R3 genügte nicht den Anforderungen der Fischgewässer-Richtlinie. Der Grenzwert für Gesamt-Phosphor wurde an S3 überschritten. In der Großen Söse war der Aluminium-Gehalt so hoch, daß anorganisches und organisches Aluminium unterschieden werden konnten. Besonders hohe Gehalte an toxischem anorganischen Aluminium wurden an Tagen mit Spitzen-Abflüssen und Versauerungsschüben gemessen. Erst die Ermittlung verschiedener chemischer Versauerungsparameter zeigte, daß auch die alkalischen Probestellen R2 und R3 mindestens versauerungsempfindlich waren. Die Messung bzw. Berechnung von chemischen Versauerungsparametern sollte deshalb zum Routineprogramm bei der Untersuchung von Gewässerversauerung gehören. Zu Beginn des Untersuchungsprogramms war angenommen worden, daß die mittleren und unteren Abschnitte der Alten Riefensbeek unversauert sind. Dieser Ansatz des Untersuchungsprogramms, einen unversauerten Referenzbach (Alte Riefensbeek) mit einem versauerten Bach (Große Söse) zu vergleichen, mußte nach der Berechnung von chemischen Versauerungsindikatoren sowie der Analyse der Abundanz- und Biomasse-Werte modifiziert werden. Es gab einen Versauerungsgradienten entlang der Probestellen: R1 (unversauert) R2 und R3 (versauerungsempfindlich bis episodisch leicht versauert) S2 und S3 (dauerhaft versauert) S1 (dauerhaft stark versauert). An S1 war das Hydrogencarbonat-Puffersystem vollständig, an S2 und S3 zeitweise ausgefallen. Die Versauerungslage an R2 und R3 war also schlechter als vorausgesehen. Unterschiede im Versauerungsgrad zwischen den Meßstellen waren nicht so sehr in unterschiedlichen Eintragsraten von versauernden Stoffen aus der Luft begründet, sondern in unterschiedlichen Grundgesteinen mit unterschiedlichem Puffervermögen. Der Anteil der verschiedenen sauren Anionen an der Versauerung wurde untersucht, die chemischen Versauerungsmechanismen wurden mit Hilfe von Ionenbilanzen und verschiedenen Versauerungsquotienten analysiert. Die beiden untersuchten Bäche waren von anthropogener Versauerung betroffen. Dabei spielte die Schwefel-Deposition (Sulfat) eine größere Rolle als die Stickstoff-Deposition (Nitrat). Die Probestelle S1 war immer schon in unbekanntem Maß natürlich sauer. Dieser natürlich saure Zustand wurde von der hinzugekommenen anthropogenen Versauerung bei weitem überragt. Die wenigen gewässerökologischen Daten, die im Wassereinzugsgebiet der Söse vor 1986 gewonnen wurden, deuten darauf hin, daß die Versauerung in den 70er und in der ersten Hälfte der 80er Jahre vom Boden und Gestein in die Bäche durchgeschlagen war. Dieser Versauerungsprozeß begann vermutlich vor 1973 in den Quellen auf dem Acker-Bruchberg und bewegte sich im Laufe der Jahre immer weiter talwärts in Richtung Trinkwasser-Talsperre. Der Mangel an (historischen) freilandökologischen Grundlagendaten war nicht nur im Untersuchungsgebiet, sondern ist allgemein in der Versauerungsforschung ein Problem. Wenn sich das Vorkommen von nah verwandten Arten (weitgehend) ausschließt, kann dies an der Versauerung liegen, z.B. war die Alte Riefensbeek ein Gammarus-Bach, die Große Söse ein Niphargus-Bach; dieses muß aber nicht an der Versauerung liegen, z.B. fehlte Habroleptoides confusa im Hyporheos an R3, Habrophlebia lauta hatte dagegen ihr Abundanz- und Biomasse-Maximum an R3. Zugleich lag das Maximum des prozentualen Anteils von Grobsand an R3, eine mögliche Ursache für diese interspezifische Konkurrenz. Die biologische Indikation von Gewässerversauerung mit Hilfe der Säurezustandsklassen funktionierte nicht in den beiden Harzbächen. Es wurde deshalb ein biologischer Versauerungsindex vorgeschlagen; dieser wurde nicht am pH-Wert kalibriert, sondern an der chemischen Versauerungslage, gekennzeichnet durch die Alkalinität und andere chemische Meßgrößen der Versauerung. Dafür wurden aufgrund der qualitativen und quantitativen Daten die häufigeren Taxa in die vier Klassen deutlich versauerungsempfindlich, mäßig versauerungsempfindlich, mäßig versauerungstolerant und deutlich versauerungstolerant eingeteilt. Es reicht nicht aus, die biologischen Folgen von Gewässerversauerung sowie Veränderungen in der Nährstoff-Verfügbarkeit und im sonstigen Wasserchemismus nur anhand der Artenzahl oder des Artenspektrums abzuschätzen. Vielmehr müssen quantitative Methoden wie die Ermittlung der Abundanzen angewandt werden, um anthropogene und natürliche Störungen des Ökosystems zu erfassen. Es wurde eine Strategie für die behördliche Gewässergüteüberwachung von Bachoberläufen vorgeschlagen, die flächendeckend die Versauerungsgefährdung erfassen kann. Die Auswirkungen der zeitlichen Dynamik des Versauerungschemismus wurden am Beispiel des versauerungsempfindlichen Taxons Baetis spp. (Eintagsfliegen) dargestellt. An S2 und S3 kam es zu starken Versauerungsschüben. Baetis konnte sich nicht ganzjährig halten, sondern nur in versauerungsarmen Phasen im Sommer und im Herbst; es gab einen Besiedlungskreislauf aus Ausrottungs- und Wiederbesiedlungsphasen. Die temporäre Population von Baetis an S2 und S3 bestand nur aus ersten Larvenstadien. Die Probestellen wurden auf horizontalen Gradienten der Umweltfaktoren angeordnet. Bei einigen Parametern gab es keinen Gradienten (z.B. Sauerstoff-Gehalt), bei anderen Parametern waren die Meßstellen auf sehr flachen Gradienten angeordnet (z.B. C:N-Quotient der Feinstkörner), bei den restlichen Meßgrößen waren die Gradienten sehr deutlich (z.B. Alkalinität). Bei den Längsgradienten von Abundanz und Biomasse waren alle Möglichkeiten vertreten: Zunahme (z.B. Leuctra pseudosignifera), Abnahme (z.B. Gammarus pulex), Maximum an der mittleren Probestelle (z.B. Leuctra pseudocingulata) und kein signifikanter Trend (z.B. Nemoura spp.). Abundanz und Biomasse zahlreicher taxonomischer Einheiten hatten ihr Maximum im Längslauf an den quellnächsten Probestellen R1 und S1, z.B. Protonemura spp. und Plectrocnemia spp. Die Lebensgemeinschaften an R1 und S1 waren allerdings völlig unterschiedlich zusammengesetzt. Die häufig vertretene Annahme, versauerte Gewässer seien biologisch tot, ist falsch. Unter Anwendung des 3. biozönotischen Grundprinzips wurde das Maximum von Abundanz und Biomasse in den quellnahen Abschnitten mit dem eustatistischen (stabilen) Regime von Wassertemperatur, Abfluß und Protonen-Gehalt, in der Alten Riefensbeek auch von Alkalinität und ALMER-Relation erklärt. Aufgrund der natürlichen und anthropogenen Störungen war im Längslauf der untersuchten Bäche keine natürliche biozönotische Gliederung des Artenbestands erkennbar. Die Korrelationsberechnungen zwischen den Umweltfaktoren und der Taxazahl ergaben, daß in erster Linie versauerungsrelevante Parameter -- Gehalte saurer Anionen, basischer Kationen und von Metallen, Alkalinität usw. -- die höchsten Korrelationskoeffizienten mit der Taxa-Zahl hatten; unter den natürlichen Meßgrößen zählten nur die Gehalte von DOC und TIC sowie der Anteil der Sande zu der Gruppe mit den höchsten Korrelationskoeffizienten. Die Korrelationsberechnungen zwischen den Umweltfaktoren und den Abundanzen ergab dagegen, daß die quantitative Zusammensetzung der Lebensgemeinschaft nicht nur durch die anthropogene Gewässerversauerung, sondern mindestens genauso durch einige natürliche Meßgrößen beeinflußt wurde. Es gab in den Harzbächen keinen ökologischen Superfaktor, der die quantitative Zusammensetzung der Lebensgemeinschaft überwiegend bestimmte. Auch die Meßgrößen der anthropogenen Gewässerversauerung waren nicht solch ein Superfaktor. Einen ähnlich hohen Einfluß auf die quantitative Zusammensetzung der Lebensgemeinschaft hatten die geologisch bestimmten Umweltfaktoren Leitfähigkeit und TIC-Gehalt, der von der Landnutzung bestimmte DOC-Gehalt sowie der Chlorid-Gehalt, der geologisch, möglicherweise aber auch durch den Eintrag von Straßensalz bestimmt wird. Die Mischung von anthropogenen und natürlichen Faktoren wurde in einem Modell der Wirkung von abiotischen Faktoren auf Bryorheos und Hyporheos dargestellt. Als Beispiel für die zeitliche Nutzung ökologischer Nischen wurde die Verteilung der Larven und Adulten der Dryopidae (Hakenkäfer) im Hyporheos und Bryorheos untersucht. Die Larven wurden vorzugsweise im Hyporheon, die Adulten im Bryorheon angetroffen. Die untersuchten Taxa wurden in die Varianten bryorheobiont, bryorheophil, bryorheotolerant, bryorheoxen und bryorheophob bzw. hyporheobiont, hyporheophil, hyporheotolerant, hyporheoxen und hyporheophob eingeteilt, um ihre räumliche Nutzung ökologischer Nischen zu beschreiben. Die gängige Lehrmeinung, daß das Hyporheon die Kinderstube benthaler Makroinvertebraten ist, konnte für zahlreiche Taxa bestätigt werden (z.B. Habrophlebia lauta). Für die bryorheophilen Taxa (z.B. Gammarus pulex und Baetis spp.) trifft diese Lehrmeinung in den beiden Harzbächen nicht zu. Vielmehr übernimmt das Bryorheon die Funktion einer Kinderstube. Die Larven von Plectrocnemia conspersa / geniculata sowie von Baetis spp. und Amphinemura spp. / Protonemura spp. neben Gammarus pulex zeigten eine Habitatbindung, die erstgenannte Gattung an das Hyporheal, die letztgenannten 3 Taxa an untergetauchte Moospolster (Bryorheal). Die Idee von der Funktion des Hyporheals als Kinderstube der Larven und Jungtiere, als Schutzraum gegen die Verdriftung durch Strömung und vor Fraßdruck durch Räuber sowie als Ort hohen Nahrungsangebots mußte für die letztgenannten 3 Taxa abgelehnt werden. Für sie übernahm das Bryorheal diese Aufgaben. Zwar waren die beiden Bäche oligotroph und die Nahrungsqualität der Feinstkörner im Hyporheal war niedrig. Die Abundanz- und Biomasse-Werte im Bryorheos und Hyporheos gehörten aber zu den weltweit höchsten. Es wurde das Paradoxon diskutiert, daß im Hyporheon der beiden Bäche Diatomeen-Rasen gefunden wurden, obwohl das Hyporheon lichtlos sein soll. Das Hyporheon wurde als ein Ökoton zwischen Benthon / Rheon und Stygon angesehen. Es wurden vier Haupttypen des Hyporheons beschrieben. Wegen des sehr unterschiedlichen Charakters des Hyporheons in verschiedenen Fließgewässern gibt es keinen einheitlichen Satz von abiotischen und biotischen Faktoren, mit denen das Hyporheon vom Benthon und Stygon abgegrenzt werden kann. In den beiden Harzbächen ähnelte das Hyporheon mehr dem Benthon als dem Stygon. Es konnte nicht anhand der chemischen Meßgrößen vom Benthon abgegrenzt werden, sondern anhand der physikalischen Meßgrößen Trübung und der Anteile von Feinsand und Schluffe/Tone sowie anhand der biologischen Parameter Summen-Abundanz und Summen-Biomasse. Aus der Typologie des Hyporheons folgt, daß ein bestimmtes Hyporheon nicht alle in der Literatur beschriebenen Funktionen innerhalb der Fließgewässer-Aue übernehmen kann. Es wurde ein Schema entwickelt, mit dem sich die optimale Liste der Parameter für die Untersuchung eines bestimmten Hyporheons auswählen läßt. Der Tendenz in der Fließgewässer-Ökologie, immer neue Konzepte zu entwickeln, die allgemeingültig sein sollen, wurde das Konzept vom individuellen Charakter von Fließgewässer-Ökosystemen entgegengestellt.