Multi-site time-trend analysis of soil fertility management effects on crop production in sub-Saharan West Africa

Soil fertility constraints to crop production have been recognized widely as a major obstacle to food security and agro-ecosystem sustainability in sub-Saharan West Africa. As such, they have led to a multitude of research projects and policy debates on how best they should be overcome. Conclusions, based on long-term multi-site experiments, are lacking with respect to a regional assessment of phosphorus and nitrogen fertilizer effects, surface mulched crop residues, and legume rotations on total dry matter of cereals in this region. A mixed model time-trend analysis was used to investigate the effects of four nitrogen and phosphorus rates, annually applied crop residue dry matter at 500 and 2000 kg ha^-1, and cereal-legume rotation versus continuous cereal cropping on the total dry matter of cereals and legumes. The multi-factorial experiment was conducted over four years at eight locations, with annual rainfall ranging from 510 to 1300 mm, in Niger, Burkina Faso, and Togo. With the exception of phosphorus, treatment effects on legume growth were marginal. At most locations, except for typical Sudanian sites with very low base saturation and high rainfall, phosphorus effects on cereal total dry matter were much lower with rock phosphate than with soluble phosphorus, unless the rock phosphate was combined with an annual seed-placement of 4 kg ha^-1 phosphorus. Across all other treatments, nitrogen effects were negligible at 500 mm annual rainfall but at 900 mm, the highest nitrogen rate led to total dry matter increases of up to 77% and, at 1300 mm, to 183%. Mulch-induced increases in cereal total dry matter were larger with lower base saturation, reaching 45% on typical acid sandy Sahelian soils. Legume rotation effects tended to increase over time but were strongly species-dependent.

Phosphorus placement an acid arenosols of the West African Sahel

Phosphorus (P) deficiency is a major constraint to pearl millet (Pennisetum glaucum L.) growth on acid sandy soils of the West African Sahel. To develop cost-effective fertilization strategies for cash poor farmers, experiments with pearl millet were conducted in southwestern Niger. Treatments comprised single superphosphate hill-placed at rates of 1, 3, 5 or 7 kg P ha^−1 factorially combined with broadcast P at a rate of 13 kg ha^−1. Nitrogen was applied as calcium ammonium nitrate at rates of 30 and 45 kg ha^−1. At low soil moisture, placement of single superphosphate in immediate proximity to the seed reduced seedling emergence. Despite these negative effects on germination, P placement resulted in much faster growth of millet seedlings than did broadcast P. With P application, potassium nutrition of millet was improved and seedling nitrogen uptake increased two- to three-fold, indicating that nitrogen was not limiting early millet growth. Averaged over the 1995 and 1996 cropping seasons, placed applications of 3, 5 and 7 kg P ha^−1 led to 72%, 81% and 88% respectively, of the grain yield produced by broadcasting 13 kg P ha^−1. Nitrogen application did not show major effects on grain yield unless P requirements were met. A simple economic analysis revealed that the profitability of P application, defined as additional income per unit of fertilizer, was highest for P placement at 3 and 5 kg ha^−1.

Vegetation changes in a river oasis on the southern rim of the Taklamakan Desert in China between 1956 and 2000

The indigenous vegetation surrounding the river oases on the southern rim of the Taklamakan Desert has drastically diminished due to overexploitation as a source of fodder, timber and fuel for the human population. The change in the spatial extent of landscape forms and vegetation types around the Qira oasis was analyzed by comparing SPOT satellite images from 1998 with aerial photographs from 1956. The analysis was supplemented by field surveys in 1999 and 2000. The study is part of a joint Chinese-European project with the aim of assessing the current state of the foreland vegetation, of gathering information on the regeneration potential and of suggesting procedures for a sustainable management. With 33 mm of annual precipitation, plants can only grow if they have access to groundwater, lakes or rivers. Most of the available water comes into the desert via rivers in the form of seasonal flooding events resulting from snow melt in the Kun Lun Mountains. This water is captured in canal systems and used for irrigation of arable fields. Among the eight herbaceous and woody vegetation types and the type of open sand without any plant life that were mapped in 2000 in the oasis foreland, only the latter, the oasis border between cultivated land and open Populus euphratica forests and Tamarix ramosissima-Phragmites australis riverbed vegetation could be clearly identified on the photographs from 1956. The comparison of the images revealed that the oasis increased in area between 1956 and 2000. Shifting sand was successfully combated near to the oasis borders but increased in extent at the outward border of the foreland vegetation. In contrast to expectations, the area covered with Populus trees was smaller in 1956 than today due to some new forests in the north of the oasis that have grown up since 1977. Subfossil wood and leaf remnants of Populus euphratica that were found in many places in the foreland must have originated from forests destroyed before 1956. In the last 50 years, the main Qira River has shifted its bed significantly northward and developed a new furcation with a large new bed in 1986. The natural river dynamics are not only an important factor in forming the oasis’ landscape but also in providing the only possible regeneration sites for all occurring plant species. The conclusion of the study is that the oasis landscape has changed considerably in the last 50 years due to natural floodings and to vegetation degradation by human overexploitation. The trend towards decreasing width of the indigenous vegetation belt resulting from the advancing desert and the expansion of arable land is particularly alarming because a decrease in its protective function against shifting sand can be expected in the future.

Cereal/legume rotation effects on rhizosphere bacterial community structure in West African soils

The increased use of cereal/legume crop rotation has been advocated as a strategy to increase cereal yields of subsistence farmers in West Africa, and is believed to promote changes in the rhizosphere that enhance early plant growth. In this study we investigated the microbial diversity of the rhizoplane from seedlings grown in two soils previously planted to cereal or legume from experimental plots in Gaya, Niger, and Kaboli, Togo. Soils from these legume rotation and continuous cereal plots were placed into containers and sown in a growth chamber with maize (Zea mays L.), millet (Pennisetum glaucum L.), sorghum (Sorghum bicolor L. Moench.), cowpea (Vigna unguiculata L.) or groundnut (Arachis hypogaea L.). At 7 and 14 days after sowing, 16S rDNA profiles of the eubacterial and ammoniaoxidizing communities from the rhizoplane and bulk soil were generated using denaturing gradient gel electrophoresis (DGGE). Community profiles were subjected to peak fitting analyses to quantify the DNA band position and intensities, after which these data were compared using correspondence and principal components analysis. The data showed that cropping system had a highly significant effect on community structure (p <0.005), irrespective of plant species or sampling time. Continuous cereal-soil grown plants had highly similar rhizoplane communities across crop species and sites, whereas communities from the rotation soil showed greater variability and clustered with respect to plant species. Analyses of the ammonia-oxidizing communities provided no evidence of any effects of plant species or management history on ammonia oxidizers in soil from Kaboli, but there were large shifts with respect to this group of bacteria in soils from Gaya. The results of these analyses show that crop rotation can cause significant shifts in rhizosphere bacterial communities.

Validierung von HPLC-Methoden zur Bestimmung von Polyphenolen und Carotinoiden in Möhren, Weizen und Mais unterschiedlicher Herkunft

In den vorliegenden Untersuchungen wurde der Gehalt von Carotinoiden in Weizen, Mais und Möhren sowie der Polyphenolgehalt in Möhren mit analytischen Methoden zum Nachweis dieser Substanzen gemessen. Der Gehalt der Carotinoide in Mais und der Gehalt der phenolischen Bestandteile in Möhren wurde mit Messungen mittels HPLC-Analytik gemessen. Die Methoden wurden aus literaturbekannten Verfahren abgeleitet und an die Anforderungen der untersuchten Probenmatrices angepasst und validiert. Dem Verfahren lag die Frage zugrunde, ob es möglich ist, Kulturpflanzen aus verschiedenen Anbausystemen auf der Basis des Gehaltes bestimmter sekundärer Pflanzeninhaltsstoffe zu differenzieren und aufgrund von Unterschieden im Gehalt der sekundären Pflanzeninhaltsstoffe zu klassifizieren. Die Gesamtverfahren wurden dabei gemäß der ISO 17025 validiert. Für die Messungen standen Proben aus definierten Langzeitversuchen und Erzeugerproben ausgesuchter ökologisch bzw. konventionell arbeitender Anbaubetriebe zur Verfügung. Als Grundlage für eine valide Methodeneinschätzung wurden die Messungen an codierten Proben vorgenommen. Eine Decodierung der Proben erfolgte erst nach der Vorlage der Messergebnisse in den genannten Projekten. Die Messung und Auswertung des Carotinoidgehaltes in Weizen, Mais und Möhren vor dem Hintergrund der Differenzierung und Klassifizierung erfolgte in Proben eines Erntejahres. Die Messung des Gehaltes phenolischer Substanzen in Möhren erfolgte in Möhren aus 3 Erntejahren. Die verwendeten HPLC-Verfahren konnten in Bezug auf den analytischen Teil der Messungen in den einzelnen Verfahrensschritten Linearität, Spezifität, Präzision und Robustheit erfolgreich überprüft werden. Darüber hinaus wurden wichtige Einflussgrößen auf die Messungen bestimmt. Für die Verfahren zur photometrischen Bestimmung der Gesamtcarotinoide konnte eine Grundkalibrierung der Parameter Präzision und Linearität des Verfahrens erfolgreich durchgeführt werden. Während der Anwendung der HPLC-Methoden an codierten Proben konnten in allen untersuchten Probenmatrices quantitativ bedeutende Inhaltsstoffe nachgewiesen und identifiziert werden. Eine vollständige Identifizierung aller dargestellten Peaks konnte in den Untersuchungen der Polyphenole in Möhren und der Carotinoide in Mais nicht erfolgen. Im Hinblick auf die Frage nach der Differenzierung und Klassifizierung ergab sich in den verschiedenen Proben ein unterschiedliches Bild. Sowohl durch den Carotinoid- als auch den Polyphenolgehalt konnten einzelne Proben statistisch signifikant differenziert werden. Die Trennleistung hing dabei sowohl von den jeweiligen Komponenten als auch von der untersuchten Probenmatrix ab. Ein durchgängig höherer Gehalt sekundärer Pflanzeninhaltsstoffe in Proben aus ökologischem Anbau konnte nicht bestätigt werden. Für die Klassifizierung der Proben verschiedener Anbauvarianten und konnten multivariate statistische Methoden, wie lineare Diskriminantenanalyse (LDA) und Classification and Regression Tree (CART), erfolgreich angewandt werden. Eine Klassifizierung mit unterschiedlichen statistischen Verfahren erbrachte dabei unterschiedliche Ergebnisse. In der Klassifizierung der decodierten Proben mittels LDA wirkten sich die Faktoren Sorte und Standort stärker auf das Klassifizierungsergebnis aus als der Faktor Anbausystem. Eine Klassifizierung der decodierten Proben nach dem Anbausystem wurde mit dem CART-Verfahren durchgeführt. Auf dieser Basis wurden für die Polyphenole in Möhren 97 % der Proben richtig klassifiziert. Durch die Messwerte des Carotinoidgehaltes und des Luteingehaltes in Weizen konnte der größere Teil der Proben (90 %) korrekt klassifiziert werden. Auf der Basis des Carotinoidgehaltes in Mais wurde der Großteil der Proben (95 %) korrekt nach dem Anbausystem klassifiziert. Auf der Basis des mittels HPLC gemessenen Carotinoidgehaltes in Möhren konnten die Proben 97 % korrekt klassifiziert werden (97 %). Insgesamt erscheint der Grundgedanke der Klassifizierung durch den Gehalt sekundärer Pflanzeninhaltsstoffe vielversprechend. Durch die vielfältigen Einflussgrößen auf den Sekundärstoffwechsel von Pflanzen müssten Veränderungen, die durch Sorte und Standort auftreten, über mehrere Jahre erhoben und systematisiert werden.

A note about Triticum in Oman

Little is known about the diversity of wheat (Triticum spp.) in Oman. Results of a survey conducted in two remote mountain oases of northern Oman indicate that there exists considerable morphological variation within and among the five traditional landraces of wheat cultivated. Within two of the landraces grown on irrigated terraces, 2 sized between 2 and 100 m , two new botanical wheat varieties (Triticum aestivum var. baladseetense and var. maqtaense) were identified of which the agronomic properties, in particular tolerance to drought and heat, and the nutritional value require further investigation.

Einfluss exogener und endogener Faktoren auf den Gehalt sekundärer Pflanzenstoffe (Carotinoide und Polyphenole) von Möhre (Daucus carota L.) und Weizen (Triticum aestivum L.)

Die vielfältigen Funktionen der sekundären Pflanzenstoffe sowohl im Organismus der Pflanze, als auch im Körper des Menschen bieten der Wissenschaft ein weites Betätigungsfeld. Die Carotinoide findet man in fast allen Plastiden der Pflanze und sie erfüllen dort Aufgaben in Form von Pigmenten, Antioxidantien, Hormonen und zählen außerdem zu den wichtigsten Bestandteilen des Photosyntheseapparates. Im menschlichen Organismus hingegen wirken sie als Provitamin A und in den Endverästelungen der Blutgefäße bei niedrigem Sauerstoffpartialdruck. Des Weiteren besitzen sie die Fähigkeiten freie Radikale unschädlich zu machen und wirken in vitro als Fänger von energiereichem Singulettsauerstoff. Die Polyphenole, die man zu der Stoffgruppe der Phenole zählt, befinden sich in den Randschichten von Obst, Gemüse, Getreide und anderen Samen. Ihnen obliegt die Aufgabe die darunter befindlichen Gewebe vor antioxidativem Verderb zu schützen. Im Körper des Menschen dagegen besitzen sie eine gerinnungshemmende Wirkung, schützen die Zellen vor Oxidation und üben Fähigkeiten aus, die Krebs vorbeugen können. Im Zuge dieser Literaturarbeit werden endogene und exogene Faktoren beschrieben, die auf Pflanzen allgemein und auf die Fokusprodukte Möhre (Daucus carota L.) und Weizen (Triticum aestivum L.) speziell einwirken. Die pflanzenphysiologische Herkunft und Bedeutung der sekundären Pflanzenstoffgruppen Carotinoide und Polyphenole wird dargestellt. Schließlich wird die vorhandene Literatur ausgewertet, die sich mit der Beeinflussung des Gehaltes der genannten sekundären Pflanzenstoffe in den gewählten Fokusprodukten durch exogene und endogene Faktoren beschäftigt. Die Beeinflussung des Polyphenolgehaltes in Möhre und des Carotinoid- und Polyphenolgehaltes in Weizen ist nur wenig untersucht. Dagegen ist die Beeinflussung des Carotinoidgehaltes in Möhren durch exogene und endogene Faktoren gut beschrieben. Der Faktor „Sorte“ spielt aufgrund der vorhandenen genetischen Anlagen (carotinoidreich / carotinoidarm) eine wesentliche Rolle bei der späteren Ausbildung des Carotinoidgehaltes in der Möhre. Die Reife der Möhre, die u.a. das Ergebnis des Einwirkens exogener Faktoren, wie Temperatur, Wuchsraum, verfügbare Wassermenge im Boden sowie der Niederschläge ist, beeinflusst maßgeblich den späteren Gehalt an Carotinoiden. Des Weiteren üben noch anbautechnische Maßnahmen (z.B. Düngung, Herbizidbehandlungen, Produktionstechnik) einen Einfluss auf den Carotinoidgehalt der Möhre aus. Der Phenolgehalt in Möhren wurde bisher ausschließlich auf Sortenebene verglichen. In einer Studie von Zhang & Hamauzu (2004) fand man heraus, dass der Phenol-Gehalt in den verschiedenen Geweben der Möhre von der Schale in Richtung Phloem und Xylem anstieg, während sich die antioxidantischen und radical scavening Aktivitäten auf gleiche Weise, wie der Phenol-Gehalt erhöhten und wiederum mit dem totalen Phenol-Gehalt korrelierten. Die phenolischen Extrakte verfügten über stärkere radical scavening Fähigkeiten, als die zum Vergleich herangezogenen Reinsubstanzen Chlorogensäure, Vitamin C und β-Carotin. Insgesamt wurde aufgrund dieser Studie vermutet, dass sich der höchste Gehalt an Phenolen in der Schale der Möhre befindet. Das geringe Vorliegen von Studien bezüglich des Carotinoid- und Phenolgehaltes in Weizen kann man darauf zurückführen, dass die sekundären Pflanzenstoffe im Vergleich zum Proteingehalt keine wesentliche Rolle als Qualitätsmerkmal beim Fokusprodukt Weizen spielen. Der Gehalt an Phenolen und Carotinoiden wurde bisher ausschließlich auf Sortenebene untersucht. Die Untersuchungen ergaben, dass der Gehalt an sekundären Pflanzenstoffen (Phenole, Tocopherole, Carotinoide) stark durch die Sorte beeinflusst wird.

Changes in amino acid enantiomers and microbial performance in soils from a subtropical mountain oasis in Oman abandoned for different periods

An important feature of maintaining the agricultural stability in millennia-old mountain oases of northern Oman is the temporary abandonment of terraces. To analyse the effects of a fallow period on soil microbial performance, i.e. microbial activity and microbial biomass, samples of eight terrace soils abandoned for different periods were collected in situ, assigned to four fallow age classes and incubated for 30 days in the laboratory after rewetting. The younger fallow age classes of 1 and 5 years were based on the records of the farmers’ recollections, the two older fallow age classes of 10–20 and 25–60 years according to the increase in the D -to- L ratio of valine and leucine enantiomers. The increase in these two ratios was in agreement with that of the D -to- L ratio of lysine. The strongest relationship was observed between the increase in the D -to- L ratio of lysine and the decrease in soil microbial biomass C. However, the most stringent coherence between the increase in fallow age and soil properties was revealed by the decreases in cumulative respiration and net N mineralisation rates with decreasing availability of substrate to soil microorganisms. During the 30-day incubation following rewetting, relative changes in microbial activity (respiration and net N mineralisation) and microbial biomass (C and N)indices were similar in the eight terrace soils on a fallow age-class-specific level, indicating that the same basic processes occurred in all of the sandy terrace soils investigated.

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.

Effects of manure quality and application forms on soil C and N turnover of a subtropical oasis soil under laboratory conditions

Our knowledge of the agricultural sustainability of the millennia-old mountain oases in northern Oman is restricted in particular with respect to C and N turnover. A laboratory study was conducted (1) to analyse the effects of rewetting and drying on soil microorganisms after adding different manures, (2) to investigate the effects of mulching or incorporating of these manures, and (3) to evaluate the relationships between C and N mineralisation rates and manure quality indices. During the first 9-day rewetting and drying cycle, i.e. the “mulch” period, the content of extractable organic C decreased by approximately 40% in all four treatments. During the second 9-day rewetting and drying cycle, i.e. the “incorporation” period, this fraction decreased insignificantly in almost all treatments. The control and mature manure treatments form the first pair with a low percentage of total organic C evolved as CO2 (0.3% in 18 days) and a considerable percentage of total N mineralised as NH4 and NO3 (1% in 18 days), the fresh and immature manure treatments form the second pair with a higher amount of total organic C evolved as CO2 (0.5% in 18 days) and no net N mineralisation. During the first 9-day rewetting and drying cycle, the contents of microbial biomass C and biomass N increased by approximately 150% in all four treatments. During the second 9-day rewetting and drying cycle, no further increase was observed in the control and immature manure treatments and a roughly 30% increase in the other two treatments.

Field measurements of the CO2 evolution rate under different crops during an irrigation cycle in a mountain oasis of Oman

For millennia oasis agriculture has been the backbone of rural livelihood in the desertic Sultanate of Oman. However, little is known about the functioning of these oasis systems, in particular with respect to the C turnover. The objective was to determine the effects of crop, i.e. alfalfa, wheat and bare fallow on the CO2 evolution rate during an irrigation cycle in relation to changes in soil water content and soil temperature. The gravimetric soil water content decreased from initially 24% to approximately 16% within 7 days after irrigation. The mean CO2 evolution rates increased significantly in the order fallow (27.4 mg C m^−2 h^−1) < wheat (45.5 mg C m^−2 h^−1) < alfalfa (97.5 mg C m^−2 h^−1). It can be calculated from these data that the CO2 evolution rate of the alfalfa root system was nearly four times higher than the corresponding rate in the wheat root system. The decline in CO2 evolution rate, especially during the first 4 days after irrigation, was significantly related to the decline in the gravimetric water content, with r = 0.70. CO2 evolution rate and soil temperature at 5 cm depth were negatively correlated (r = -0.56,n = 261) due to increasing soil temperature with decreasing gravimetric water content.

Effects of post-harvest treatments on the carbohydrate composition of yacon roots in the Peruvian Andes

Yacon (Smallanthus sonchifolius [Poepp. & Endl.] H. Robinson) is an under-exploited native root crop of the Andes, which stores oligofructans (fructo-oligosaccharides, FOS) as its main component of dry matter (DM). FOS are of increasing economic interest because of their low caloric value in human diets and bifidogenic benefits on colon health. Two on-farm experiments were conducted to: (i) determine the effect of shaded, short-term storage at 1990 and 2930 m a.s.l. in the Andean highlands; and (ii) address the effects of a traditional sunlight exposure (‘sunning’) on the carbohydrate composition in the DM of tuberous yacon roots. After a 6-day shade storage FOS concentrations were smaller at the lower (36–48% of DM) than at the higher altitude (39–58% of DM). After 12 days FOS concentrations were nearly equal at both sites (27–39% of DM). The concentration of free sugars (fructose, glucose, sucrose) increased accordingly from 29–34 to 48–52%. During the 6-day sunning experiment FOS concentrations decreased from 50–62 to 29–44% and free sugars increased from 29–34 to 45–51%. The results indicate that partial hydrolysis of oligofructans starts shortly after harvest. Storage in highland environments should wherever possible exploit the cooler temperatures at higher altitudes. Sunning of yacon’s tuberous roots effectively reduces much of the roots’ water content, in this experiment 40%, and thus allows energy to be saved if yacon is processed into dehydrated products.

Emmer (Triticum dicoccon Schrank) in Oman

Emmer (Triticum dicoccon ) was collected recently in northern Oman. The material was analyzed morphologically and phenologically. It belongs to the Asiatic emmers (subsp. asiaticum) and not to the Ethiopian ones (subsp. abyssinicum), distributed in Ethiopia and Yemen, as originally expected. The determination of the material resulted in var. haussknechtianum and var. aeruginosum.

Low-altitude aerial photography for optimum N fertilization of winter wheat on the North China Plain

Previous research has shown that site-specific nitrogen (N) fertilizer recommendations based on an assessment of a soil’s N supply (mineral N testing) and the crop’s N status (sap nitrate analysis) can help to decrease excessive N inputs for winter wheat on the North China Plain. However, the costs to derive such recommendations based on multiple sampling of a single field hamper the use of this approach at the on-farm level. In this study low-altitude aerial true-color photographs were used to examine the relationship between image-derived reflectance values and soil–plant data in an on-station experiment. Treatments comprised a conventional N treatment (typical farmers’ practice), an optimum N treatment (N application based on soil–plant testing) and six treatments without N (one to six cropping seasons without any N fertilizer input). Normalized intensities of the red, green and blue color bands on the photographs were highly correlated with total N concentrations, SPAD readings and stem sap nitrate of winter wheat. The results indicate the potential of aerial photography to determine in combination with on site soil–plant testing the optimum N fertilizer rate for larger fields and to thereby decrease the costs for N need assessments.