Effects of activated charcoal and quebracho tannins on the turnover of goat manure in irrigated organic agriculture of the subtropics

Agriculture in semi-arid and arid regions is constantly gaining importance for the security of the nutrition of humankind because of the rapid population growth. At the same time, especially these regions are more and more endangered by soil degradation, limited resources and extreme climatic conditions. One way to retain soil fertility under these conditions in the long run is to increase the soil organic matter. Thus, a two-year field experiment was conducted to test the efficiency of activated charcoal and quebracho tannin extract as stabilizers of soil organic matter on a sandy soil low in nutrients in Northern Oman. Both activated charcoal and quebracho tannin extract were either fed to goats and after defecation applied to the soil or directly applied to the soil in combination with dried goat manure. Regardless of the application method, both additives reduced decomposition of soil-applied organic matter and thus stabilized and increased soil organic carbon. The nutrient release from goat manure was altered by the application of activated charcoal and quebracho tannin extract as well, however, nutrient release was not always slowed down. While activated charcoal fed to goats, was more effective in stabilising soil organic matter and in reducing nutrient release than mixing it, for quebracho tannin extract the opposite was the case. Moreover, the efficiency of the additives was influenced by the cultivated crop (sweet corn and radish), leading to unexplained interactions. The reduced nutrient release caused by the stabilization of the organic matter might be the reason for the reduced yields for sweet corn caused by the application of manure amended with activated charcoal and quebracho tannin extract. Radish, on the other hand, was only inhibited by the presence of quebracho tannin extract but not by activated charcoal. This might be caused by a possible allelopathic effect of tannins on crops. To understand the mechanisms behind the changes in manure, in the soil, in the mineralisation and the plant development and to resolve detrimental effects, further research as recommended in this dissertation is necessary. Particularly in developing countries poor in resources and capital, feeding charcoal or tannins to animals and using their faeces as manure may be promising to increase soil fertility, sequester carbon and reduce nutrient losses, when yield reductions can be resolved.

Effect of environmental conditions on the N uptake route of soil microorganisms and adaption of a method to determine amino acid oxidase in soil

Soil microorganisms have evolved two possible mechanisms for their uptake of organic N: the direct route and the mobilization-immobilization-turnover (MIT) route. In the direct route, simple organic molecules are taken up via various mechanisms directly into the cell. In the MIT route, the deamination occurs outside the cell and all N is mineralized to NH4+ before assimilation. A better understanding of the mechanisms controlling the different uptake routes of soil microorganisms under different environmental conditions is crucial for understanding mineralization processes of organic material in soil. For the first experiment we incubated soil samples from the long term trial in Bad Lauchstädt with corn residues with different C to N ratios and inorganic N for 21 days at 20 °C. Under the assumption that all added amino acids were taken up or mineralized, the direct uptake route was more important in soil amended with corn residues with a wide C to N ratio. After 21 days of incubation the direct uptake of added amino acids increased in the order addition of corn residue with a: “C to N ratio of 40 & (NH4)2SO4 and no addition (control)” (69% and 68%, respectively) < “C to N ratio of 20” (73%) < “C to N ratio of 40” (95%). In all treatments the proportion of the added amino acids that were mineralized increased with time, indicating that the MIT route became more important over time. To investigate the effects of soil depth on the N uptake route of soil microorganisms (experiment II), soil samples in two soil depths (0-5 cm; 30-40 cm) were incubated with corn residues with different C to N ratios and inorganic N for 21 days at 20 °C and 60% (WHC). The addition of corn residue resulted in a marked increase of protease activity in both depths due to the induction from the added substrate. Addition of corn residue with a wide C to N ratio resulted in a significantly greater part of the direct uptake (97% and 94%) than without the addition of residues (85% and 80%) or addition of residue with a small C to N ratio (90% and 84%) or inorganic N (91% and 79% in the surface soil and subsoil, respectively), suggesting that under conditions of sufficient mineralizable N (C to N ratio of 20) or increased concentrations of NH4+, the enzyme system involved in the direct uptake is slightly repressed. Substrate additions resulted in an initially significantly higher increase of the direct uptake in the surface soil than in the subsoil. As a large proportion of the organic N input into soil is in form of proteinaceous material, the deamination of amino acids is a key reaction of the MIT route. Therefore the enzyme amino acid oxidase contribute to the extracellular N mineralization in soil. The objective of experiment III was to adapt a method to determine amino acid oxidase in soil. The detection via synthetic fluorescent Lucifer Yellow derivatives of the amino acid lysine is possible in soil. However, it was not possible to find the substrate concentration at which the reaction rate is independent of substrate concentration and therefore we were not able to develop a valid soil enzyme assay.

Microbial response to restoration of tantalite mine soils in western Rwanda

Artisanal columbite-tantalite (coltan) mining has had negative effects on the rural economy in the great Lakes region of Africa through labor deficits, degradation and loss of farmland, food insecurity, high cost of living, and reduced traditional export crop production alongside secondary impacts that remotely affect the quality of air, water, soil, plants, animals, and human wellbeing. The situation is multifaceted and calls for a holistic approach for short and long-term mitigation of such negative effects. This study focuses on the effects of mine land restoration on soil microbiological quality in the Gatumba Mining District of western Rwanda. Some coltan mine wastelands were afforested with pine and eucalyptus trees while farmers directly cultivated others due to land scarcity. Farmyard manure (FYM) is the sole fertilizer applied on the wastelands although it is insufficient to achieve the desired crop yields. Despite this, several multi-purpose plants such as Tithonia diversifolia, Markhamia lutea, and Canavalia brasiliensis thrive in the area and could supplement FYM. The potential for these “new” amendments to improve soil microbial properties, particularly in the tantalite mine soils was investigated. The specific objectives of the study were to: (a) evaluate the effects of land use on soil microbial indices of the tantalite mine soils; (b) investigate the restorative effects of organic amendments on a Technosol; and (c) estimate the short-term N and P supply potential of the soil amendments in the soils. Fresh soils (0-20 cm) from an unmined native forest, two mine sites afforested with pine and eucalyptus forests (pine and eucalyptus Technosols), an arable land, and two cultivated Technosols (Kavumu and Kirengo Technosols) were analyzed for the physicochemical properties. Afterwards, a 28-day incubation (22oC) experiment was conducted followed by measurements of mineral N, soil microbial biomass C, N, P, and fungal ergosterol contents using standard methods. This was followed by a 12-week incubation study of the arable soil and the Kavumu Technosol amended with FYM, Canavalia and Tithonia biomass, and Markhamia leaf litter after which soil microbial properties were measured at 2, 8, and 12 weeks of incubation. Finally, two 4-week incubation experiments each were conducted in soils of the six sites to estimate (i) potential mineralizable N using a soil-sand mixture (1:1) amended with Canavalia and goat manure and (ii) P mineralization mixtures (1:1) of soil and anion exchange resins in bicarbonate form amended with Tithonia biomass and goat manure. In study one, afforestation increased soil organic carbon and total N contents in the pine and eucalyptus Technosols by 34-40% and 28-30%, respectively of that in the native forest soil. Consequently, the microbial biomass and activity followed a similar trend where the cultivated Technosols were inferior to the afforested ones. The microbial indices of the mine soils were constrained by soil acidity, dithionite-extractable Al, and low P availability. In study two, the amendments substantially increased C and N mineralization, microbial properties compared with non-amended soils. Canavalia biomass increased CO2 efflux by 340%, net N mineralization by 30-140%, and microbial biomass C and N by 240-600% and 240-380% (P < 0.01), respectively after four weeks of incubation compared with the non-amended soils. Tithonia biomass increased ergosterol content by roughly 240%. The Kavumu Technosol showed a high potential for quick restoration of its soil quality due to its major responses to the measured biological parameters. In study three, Canavalia biomass gave the highest mineralizable N (130 µg g-1 soil, P < 0.01) in the Kavumu Technosol and the lowest in the native forest soil (-20 µg g-1 soil). Conversely, the mineralizable N of goat manure was negative in all soils ranging from -2.5 µg N g-1 to -7.7 µg N g-1 soil except the native forest soil. However, the immobilization of goat manure N in the “cultivated soils” was 30-70% lower than in the “forest soils” signifying an imminent recovery of the amended soils from N immobilization. The mineralization of goat manure P was three-fold that of Tithonia, constituting 61-71% of total P applied. Phosphorus mineralization slightly decreased after four weeks of incubation due to sulfate competition as reflected in a negative correlation, which was steeper in the Tithonia treatment. In conclusion, each amendment used in this research played a unique role in C, N, and P mineralization and contributed substantially to microbial properties in the tantalite mine soils. Interestingly, the “N immobilizers” exhibited potentials for P release and soil organic carbon storage. Consequently, the combined use of the amendments in specific ratios, or co-composting prior to application is recommended to optimize nutrient release, microbial biomass dynamics and soil organic matter accrual. Transport of organic inputs seems more feasible for smallholder farmers who typically manage small field sizes. To reduce acidity in the soils, liming with wood ash was recommended to also improve P availability and enhance soil biological quality, even if it may only be possible on small areas. Further, afforestation with mixed-species of fast-growing eucalyptus and legume or indigenous tree species are suggested to restore tantalite mine wastelands. It is emphasized most of this research was conducted under controlled laboratory conditions, which exclude interaction with environmental variables. Also fine fractions of the amendments were used compared with the usual practice of applying a mixture of predominantly coarser fractions. Therefore, the biological dynamics reported in the studies here may not entirely reflect those of farmers’ field conditions.

Impacto funcional con el uso de clavo telescopico tipo Fassier Duval en pacientes con osteogénesis imperfecta

Introducción: la osteogénesis es una patología de origen genético caracterizada por fragilidad ósea, en su curso natural los pacientes que la padecen se enfrentan a múltiples fracturas y múltiples intervenciones quirúrgicas, este tipo de pacientes por ser de alto riesgo necesitan técnicas quirúrgicas que aumenten el tiempo entre cada intervención y que demuestren un mayor impacto en el estado funcional. Objetivo: Determinar el impacto en el estado funcional de los pacientes con osteogénesis imperfecta llevados a tratamiento quirúrgico con clavos telescopados tipo Fassier Duval. Diseño: Estudio descriptivo prospectivo en el que se incluyeron 8 pacientes con diagnóstico de osteogénesis imperfecta, llevados a tratamiento quirúrgico con clavos telescopados tipo Fassier Duval desde el 2009 al 2013 a los cuales se les realizó seguimiento menor de 1 año del post operatorio. Resultados: La respuesta encontrada fue satisfactoria en la mayoría de los pacientes analizados 6 de 8, con cercanía a un estado funcional normal; un riesgo de caída bajo, incorporación y deambulación adecuada y una valoración funcional motora gruesa con valores cercanos al 100% identificando un buen nivel de independencia funcional. Se pudo demostrar que existieron cambios en los valores de la escala y que estos fueron estadísticamente significativos con p=0,028 indicando que el aumento dichos valores en el posoperatorio están relacionados con el procedimiento quirúrgico al utilizado en este grupo de pacientes. Conclusión: El tratamiento quirúrgico con el clavo telescopado de Fassier Duval en nuestra experiencia demostró tener una mejoría en el estado funcional de los pacientes del presente estudio, por lo tanto se sugiere la posibilidad de implementar su uso según este indicado con el fin de obtener un mejor resultado quirúrgico y funcional. Palabras clave: Osteogénesis Imperfecta, Clavo de Fassier Duval, Valoración Funcional Motora

La reeducación : un tratamiento psicodinámico de los trastornos del aprendizaje.

Se muesta la reflexión de la experiencia clínica de los autores con la voluntad de abrir vías terapéuticas que faciliten el abordaje de los trastornos del aprendizaje. Se trata de prestar mayor atención al trasfondo emocional y personal del niño. El enfoque se basa en establecer un vínculo relacional con el niño a fin de captar sus sentimientos y motivaciones para así establecer una verdadera comunicación con él. Todo ello a través actividades, que al despertar el interés del niño, facilitan la permeabilidad de la capacidad de aprender.

Toby's funfair fish.

A Toby le encanta ir a la feria y está más entusiasmado que de costumbre porque se ha ganado un pez de colores. Nunca tuvo una mascota antes y está muy emocionado con su pescado Moby. Para que Moby sea feliz y se sienta como en casa, le hace en la pecera su propio recinto ferial.

Cosmo and the magic sneeze.

La historia de un gatito blanco y negro llamado Cosmo y sus padres, India y Mephisto. Mephisto es un gato de brujas, un gato que puede utilizar su magia para ayudar a estornudar a una bruja en sus hechizos, mientras que India es un gato doméstico normal. Cosmo tiene que pasar una prueba especial para ver si es más como Mephisto o India. Cuando pasa la prueba especial, es capaz de ayudar a estornudar a la bruja Sybil y llevar a cabo la magia estornudo que añade el ingrediente extra-especial al caldero. Sybil y su madre, Eufemia, están haciendo una poción secreta para un hechizo que produce estatuas de oro y Scarlett, Bunty y Cosmo tienen que averiguar cuáles son los componentes de la poción, antes de que sea demasiado tarde. Sobre todo porque las estatuas tienen forma de gatitos.

OCR British depth study, 1939-1975.

Su contenido ha sido aprobado por el organismo Oxford Cambridge and RSA Examinations (OCR) para obtener el título de General Certificate Secondary Education (GCSE) en la especificación de Historia del mundo moderno. Está dividido en tres partes que proporcionan asesoramiento para enfocar el examen; los conocimientos contextuales para trabajar con las fuentes en los temas propuestos y, por último, modelos de examen para investigar sobre las fuentes.

France in revolution.

Se adapta su contenido a las especificaciones AS y A2 de 2008 de todos los tribunales examinadores. Estudia las causas de la Revolución Francesa, su impacto político, social y económico y el establecimiento del Terror. También, se incluye un capítulo adicional sobre el dominio napoleónico en Francia entre 1799 y 1815. Contiene fechas clave, términos y temas, perfiles biográficos, resúmenes esquemáticos, fuentes literarias y síntesis de los principales debates historiográficos.

Napoleon, France and Europe.

Su contenido se adapta a las especificaciones AS y A2 para Edexcel y OCR. Traza los cambios que tuvieron lugar en Francia entre 1795 y 1815. Estudia la subida de Napoleón al poder, su consolidación y mantenimiento, así como la creación del Imperio napoleónico y su caída. Incluye fechas clave, términos y temas, perfiles biográficos, resúmenes esquemáticos, fuentes literarias y síntesis de los principales debates historiográficos sobre las políticas de Napoleón.

ICT Interact for KS3 : pupil's book and cd 2.

Libro para estudiantes de enseñanza secundaria - primer ciclo (Key Stage 3) en el área de las tecnologías de la información y la comunicación. Está estructurado en siete módulos que a su vez se dividen en unidades, y que el profesor puede combinar de forma flexible para adaptarse a los intereses de los alumnos. Incluye un cd-rom con recursos de apoyo y una copia electrónica del libro por cuyos contenidos se puede navegar. Los temas que se cubren son: localización y presentación de la información, diseño y creación Web y tratamiento de datos.

Procesos y contextos educativos : enseñar en las instituciones de Educación Secundaria.

Resumen basado en el de la publicación

Cómo ser docente sin perder la salud ni el buen humor.

Este artículo pertenece a una sección de la revista dedicada a innovación educativa, en este número a salud laboral. - Resumen tomado parcialmente de la revista

Decomposition in soil and chemical characteristics of pollen

The input to soils made by pollen and its subsequent mineralization has rarely been investigated from a soil microbiological point of view even though the small but significant quantities of C and N in pollen may make an important contribution to nutrient cycling. The relative resistance to decomposition of pollen exines (outer layers) has led to much of the focus of pollen in soil being on its preservation for archaeological and palaeo-ecological purposes. We have examined aspects of the chemical composition and decomposition of pollen from birch (Betula alba) and maize (Zea mays) in soil. The relatively large N contents, small C-to-N ratios and large water-soluble contents of pollen from both species indicated that they would be readily mineralized in soil. When added to soil and incubated at 16 degrees C an amount of C equivalent to 22-26% of the added pollen C was lost as CO2 within 22 days, with the Z. mays pollen decomposing faster. For B. alba pollen, the water-soluble fraction decomposed faster than the whole pollen and the insoluble fraction decomposed more slowly over 22 days. By contrast, there were no significant differences in the decomposition rates of the different fractions from Z. mays pollen. Solid-state C-13 nuclear magnetic resonance (NMR) revealed no gross chemical differences between the pollen of these two species, with strong resonances in the alkyl- and methyl-C region (0-45 p.p.m.) indicative of aliphatic compounds, the O-alkyl-C (60-90 p.p.m.) and the acetal- and ketal-C region (90-110 p.p.m.) indicative of polysaccharides, and the carbonyl-C region indicative of peptides and carboxylic acids. In addition, both pollens gave a small but distinct resonance at 55 p.p.m. attributed to N-alkyl-C. The resonances attributed to polysaccharides were lost completely or substantially reduced after decomposition.

Modeling the mechanisms that control in-stream dissolved organic carbon dynamics in upland and forested catchments

[1] We present a new, process-based model of soil and stream water dissolved organic carbon (DOC): the Integrated Catchments Model for Carbon (INCA-C). INCA-C is the first model of DOC cycling to explicitly include effects of different land cover types, hydrological flow paths, in-soil carbon biogeochemistry, and surface water processes on in-stream DOC concentrations. It can be calibrated using only routinely available monitoring data. INCA-C simulates daily DOC concentrations over a period of years to decades. Sources, sinks, and transformation of solid and dissolved organic carbon in peat and forest soils, wetlands, and streams as well as organic carbon mineralization in stream waters are modeled. INCA-C is designed to be applied to natural and seminatural forested and peat-dominated catchments in boreal and temperate regions. Simulations at two forested catchments showed that seasonal and interannual patterns of DOC concentration could be modeled using climate-related parameters alone. A sensitivity analysis showed that model predictions were dependent on the mass of organic carbon in the soil and that in-soil process rates were dependent on soil moisture status. Sensitive rate coefficients in the model included those for organic carbon sorption and desorption and DOC mineralization in the soil. The model was also sensitive to the amount of litter fall. Our results show the importance of climate variability in controlling surface water DOC concentrations and suggest the need for further research on the mechanisms controlling production and consumption of DOC in soils.