Amelioration of a degraded acid soil from SW Spain by no-tillage and Ca-amendment

En los suelos, el exceso de acidez lleva asociado deficiencias en ciertos nutrientes y una alta disponibilidad de aluminio, tóxico para los cultivos propios del ambiente mediterráneo. Su laboreo, provoca la pérdida de materia orgánica (MO), deteriora su estructura y reduce la actividad biológica, provocando en última instancia una menor calidad del suelo. Es de esperar pues que cuando se labran suelos ácidos, sus problemáticas particulares tiendan a agravarse. En nuestra zona de estudio, la “raña” de Cañamero (Extremadura, España), predominan los suelos muy ácidos y degradados por un laboreo inadecuado. Las rañas constituyen amplias plataformas casi horizontales, con unos suelos muy viejos (Palexerults), que se caracterizan por tener el complejo de cambio dominado por el aluminio, y un pH ácido que decrece en profundidad. Poseen un potente horizonte Bt rico en arcillas caoliníticas, que propicia que en periodos con exceso de lluvia, se generen capas colgadas de agua cercanas a la superficie. En torno a los años 1940’s estos suelos, que previamente sostenían un alcornocal, o su matorral de sustitución, se pusieron en cultivo. El laboreo aceleró la mineralización de la materia orgánica, agravó los problemas derivados del exceso de acidez y condujo al abandono de los campos cultivados por falta de productividad. Para recuperar la calidad de estos suelos degradados y obtener unos rendimientos compatibles con su uso agrícola es necesario, por un lado, aplicar enmiendas que eleven el pH y reduzcan la toxicidad del aluminio y, por otro, favorecer el incremento en el contenido en MO. En 2005 se implantó en esta raña un ensayo de campo para estudiar la influencia del no laboreo y de la utilización de una enmienda cálcica en parámetros relacionados con la calidad del suelo en un cultivo forrajero. El diseño experimental fue en parcelas divididas con cuatro repeticiones donde el factor principal fue el tipo de laboreo, no laboreo (NL) frente a laboreo convencional (LC), y el factor secundario el uso o no de una enmienda cálcica. La enmienda consistió básicamente en una mezcla de espuma de azucarería y yeso rojo y se incorporó al comienzo del ensayo hasta los 7 cm de profundidad. Desde el comienzo del ensayo el NL influyó positivamente en el contenido de carbono orgánico total (COT) y particulado (COP), mientras que la enmienda tuvo una ligera influencia al principio del ensayo en ambos pero su efecto positivo se desvaneció con el paso del tiempo. Los mayores contenidos en COT y POC se observaron cuando se combinó el NL con la enmienda. La enmienda incrementó con rapidez el pH, y el Ca, y disminuyó el contenido en aluminio hasta una profundidad de 50 cm, incluso en NL, y mejoró ligeramente la agregación del suelo. El NL por sí solo, gracias al aumento en POC, TOC y las proteínas del suelo relacionadas con la glomalina (PSRG), que son capaces de formar compuestos estables no tóxicos con el aluminio, también contribuyó a la reducción de la toxicidad de aluminio en la capa más superficial. Cuando en las campañas con exceso de precipitaciones se generaron capas colgadas de agua próximas a la superficie, el NL generó unas condiciones más favorables para la germinación y desarrollo del cultivo, resultando en una producción más alta que el LC. A ello contribuyó la mayor capacidad de almacenamiento de agua y la mayor transmisividad de esta hacia abajo, en la capa más superficial (0-5 cm) que propició una menor saturación por agua que el LC. Respecto a los parámetros relacionados con la agregación, el NL aumentó los macroagregados hasta los 10 cm de profundidad y favoreció la acumulación de CO y N en todas las fracciones de tamaño de agregados. Sin embargo, la recuperación del grado de macroagregación tras el cese del laboreo resulta lenta en comparación con otros suelos, posiblemente debido al bajo contenido en arcilla en el horizonte Ap. En comparación con el NL, la enmienda mostró también un efecto positivo, aunque muy ligero, en la agregación del suelo. En contradicción con otros estudios en suelos ácidos, nuestros resultados indican la existencia de una jerarquía de agregados, y destacan el papel importante de la MO en la mejora de la agregación. Tanto el NL como la enmienda favorecieron por separado varias propiedades químicas, físicas y biológicas del suelo, pero, en general, encontramos los mayores beneficios con su uso combinado. Además, a largo plazo el efecto positivo de NL en las propiedades del suelo fue en aumento, mientras que el efecto beneficioso de la enmienda se limitó básicamente a las propiedades químicas y se desvaneció en pocos años. Destacamos que las condiciones meteorológicas a lo largo del ensayo beneficiaron la producción de biomasa en NL, y en consecuencia las propiedades relacionadas con la materia orgánica, por lo que son un factor a tener en cuenta a la hora de evaluar los efectos de la enmienda y el laboreo sobre las propiedades del suelo, especialmente en zonas donde esas condiciones son muy variables entre una campaña y otra. Los resultados de este estudio han puesto de manifiesto que el NL no ha mermado la eficacia de la enmienda caliza, posiblemente gracias a la alta solubilidad de la enmienda aplicada, es más, el manejo con NL y enmienda es el que ha favorecido en mayor medida ciertos parámetros de calidad del suelo. Por el contrario el LC sí parece anular los beneficios de la enmienda en relación con las propiedades relacionadas con la MO. Por tanto, cabe concluir que la combinación de NL y la enmienda es una práctica adecuada para mejorar las propiedades químicas y físicas de suelos ácidos degradados por el laboreo. ABSTRACT Excessive acidity in soils is associated with deficiencies in certain nutrients and high concentrations of available aluminum, which is toxic for most Mediterranean crops. Tilling these soils results in the loss of soil organic matter (SOM), damages soil structure and reduces biological activity, ultimately degrading soil quality. It is expected, therefore, that when acid soils are tilled, their particular problems will tend to get worse. In our study area, the "Cañamero’s Raña” (Extremadura, Spain), acid soils degraded by an inappropriate tillage prevail. Rañas are large and flat platforms with very old soils (Palexerults), which are characterized by an exchange complex dominated by aluminum and an acid pH which decreases with depth. These soils have a strong Bt horizon rich in kaolinite clays, which encourages the formation of perched water-tables near the soil surface during periods of excessive rain. During the first third of the 20th century, these soils, that previously supported cork oak or its scrub replacement, were cultivated. Tillage accelerated the mineralization of the SOM, aggravating the problems of excessive acidity, which finally led to the abandonment of the land due to low productivity. To recover the quality of these degraded soils and to obtain consistent yields it is necessary, first, to apply amendments to raise the pH and reduce aluminum toxicity, and second to encourage the accumulation of SOM. In 2005 a field trial was established in the Raña to study the influence of no-tillage and the use of a Ca-amendment on soil quality related parameters in a forage crop agrosystem. The experimental design was a split-plot with four replicates where the main factor was tillage type, no-tillage (NT) versus traditional tillage (TT) and the secondary factor was the use or not of a Ca-amendment. The Ca-amendment was a mixture of sugar foam and red gypsum that was incorporated into the top 7 cm of the soil. Since the beginning of the experiment, NT had a positive influence on total and particulate organic carbon (TOC and POC, respectively), while the Ca-amendment had a small positive influence at the beginning of the study but its effect diminished with time. The highest TOC and POC contents were observed when NT and the Ca-amendment were combined. The Ca-amendment, even under NT, rapidly increased pH and Ca, and decreased the aluminum content to a depth of 50 cm, as well as improving soil aggregation slightly. NT, due to the increased POC, TOC and Glomalin-related soil proteins (GRSP), which can form stable non-toxic compounds with aluminum, also contributed to the reduction of aluminum toxicity in the upper layer. When perched water-tables near the soil surface were formed in campaigns with excessive rainfall, NT provided more favorable conditions for germination and crop development, resulting in higher yields compared with TT. This was directly related to the higher water storage capacity and the greater transmissivity of the water downwards from the upper layers, which led to lower water saturation under NT compared with TT. With regards to the aggregation-related parameters, NT increased macroaggregation to a depth of 10 cm and favored the accumulation of OC and N in all aggregate size fractions. However, the degree of recovery of macroaggregation after tillage ceased was slow compared with other soils, possibly due to the low clay content in the Ap horizon. Compared with NT, the Ca-amendment had a slight positive effect on soil aggregation. In contrast to other studies in acid soils, our results indicate the existence of an aggregate hierarchy, and highlight the important role of SOM in improving aggregation. Both NT and the Ca-amendment separately favored various chemical, physical and biological soil properties, but in general we found the greatest benefits when the two treatments were combined. In addition, the positive effect of NT on soil properties increased with time, while the beneficial effect of the Ca-amendment, which was limited to the chemical properties, vanished after a few years. It is important to note that the meteorological conditions throughout the experiment benefited biomass production under NT and, as a consequence, organic matter related properties. This suggests that meteorological conditions are a factor to consider when evaluating the effects of Ca-amendments and tillage on soil properties, especially in areas where such conditions vary significantly from one campaign to another. The results of this study show that NT did not diminish the effectiveness of the Ca-amendment, possibly due to the high solubility of the selected amendment. Moreover, the combination of NT and the Ca-amendment was actually the management that favored certain soil quality parameters the most. By contrast, TT seemed to nullify the benefits of the Ca-amendment with regards to the OM related properties. In conclusion, the combination of NT and the application of a Ca-amendment is an advisable practice for improving the chemical and physical properties of acid soils degraded by tillage.

Mejora de la eficacia de Penicillium oxalicum como agente de biocontrol en enfermedades de plantas hortícolas

Actualmente, la reducción de materias activas (UE) y la implantación de la nueva Directiva comunitaria 2009/128/ que establece el marco de actuación para conseguir un uso sostenible de los plaguicidas químicos y la preferencia de uso de métodos biológicos, físicos y otros no químicos, obliga a buscar métodos de control menos perjudiciales para el medio ambiente. El control biológico (CB) de enfermedades vegetales empleando agentes de control biológico (ACB) se percibe como una alternativa más segura y con menor impacto ambiental, bien solos o bien como parte de una estrategia de control integrado. El aislado 212 de Penicillium oxalicum (PO212) (ATCC 201888) fue aislado originalmente de la micoflora del suelo en España y ha demostrado ser un eficaz ACB frente a la marchitez vascular del tomate. Una vez identificado y caracterizado el ACB se inició el periodo de desarrollo del mismo poniendo a punto un método de producción en masa de sus conidias. Tras lo cual se inició el proceso de formulación del ACB deshidratando las conidias para su preservación durante un período de tiempo mayor mediante lecho fluido. Finalmente, se han desarrollado algunos formulados que contienen de forma individual diferentes aditivos que han alargado su viabilidad, estabilidad y facilitado su manejo y aplicación. Sin embargo, es necesario seguir trabajando en la mejora de su eficacia de biocontrol. El primer objetivo de esta Tesis se ha centrado en el estudio de la interacción ACB-patógeno-huésped que permita la actuación de P.oxalicum en diferentes patosistemas. Uno de los primeros puntos que se abordan dentro de este objetivo es el desarrollo de nuevas FORMULACIONES del ACB que incrementen su eficacia frente a la marchitez vascular del tomate. Las conidias formuladas de PO212 se obtuvieron por la adición conjunta de distintos aditivos (mojantes, adherentes o estabilizantes) en dos momentos diferentes del proceso de producción/secado: i) antes del proceso de producción (en la bolsa de fermentación) en el momento de la inoculación de las bolsas de fermentación con conidias de PO212 o ii) antes del secado en el momento de la resuspensión de las conidias tras su centrifugación. De las 22 nuevas formulaciones desarrolladas y evaluadas en plantas de tomate en ensayos en invernadero, seis de ellas (FOR22, FOR25, FOR32, FOR35, FOR36 y FOR37) mejoran significativamente (P=0,05) el control de la marchitez vascular del tomate con respecto al obtenido con las conidias secas de P.oxalicum sin aditivos (CSPO) o con el fungicida Bavistin. Los formulados que mejoran la eficacia de las conidias secas sin aditivos son aquellos que contienen como humectantes alginato sódico en fermentación, seguido de aquellos que contienen glicerol como estabilizante en fermentación, y metil celulosa y leche desnatada como adherentes antes del secado. Además, el control de la marchitez vascular del tomate por parte de los formulados de P. oxalicum está relacionado con la fecha de inicio de la enfermedad. Otra forma de continuar mejorando la eficacia de biocontrol es mejorar la materia activa mediante la SELECCIÓN DE NUEVAS CEPAS de P. oxalicum, las cuales podrían tener diferentes niveles de eficacia. De entre las 28 nuevas cepas de P. oxalicum ensayadas en cámara de cultivo, sólo el aislado PO15 muestra el mismo nivel de eficacia que PO212 (62-67% de control) frente a la marchitez vascular del tomate en casos de alta presión de enfermedad. Mientras que, en casos de baja presión de enfermedad todas las cepas de P. oxalicum y sus mezclas demuestran ser eficaces. Finalmente, se estudia ampliar el rango de actuación de este ACB a OTROS HUÉSPEDES Y OTROS PATÓGENOS Y DIFERENTES GRADOS DE VIRULENCIA. En ensayos de eficacia de P. oxalicum frente a aislados de diferente agresividad de Verticillium spp. y Fusarium oxysporum f. sp. lycopersici en plantas de tomate en cámaras de cultivo, se demuestra que la eficacia de PO212 está negativamente correlacionada con el nivel de enfermedad causada por F. oxysporum f. sp. lycopersici pero que no hay ningún efecto diferencial en la reducción de la incidencia ni de la gravedad según la virulencia de los aislados. Sin embargo, en los ensayos realizados con V. dahliae, PO212 causa una mayor reducción de la enfermedad en las plantas inoculadas con aislados de virulencia media. La eficacia de PO212 también era mayor frente a aislados de virulencia media alta de F. oxysporum f. sp. melonis y F. oxysporum f. sp. niveum, en plantas de melón y sandía, respectivamente. En ambos huéspedes se demuestra que la dosis óptima de aplicación del ACB es de 107 conidias de PO212 g-1 de suelo de semillero, aplicada 7 días antes del trasplante. Además, entre 2 y 4 nuevas aplicaciones de PO212 a la raíces de las plantas mediante un riego al terreno de asiento mejoran la eficacia de biocontrol. La eficacia de PO212 no se limita a hongos patógenos vasculares como los citados anteriormente, sino también a otros patógenos como: Phytophthora cactorum, Globodera pallida y G. rostochiensis. PO212 reduce significativamente los síntomas (50%) causados por P. cactorum en plantas de vivero de fresa, tras la aplicación del ACB por inmersión de las raíces antes de su trasplante al suelo de viveros comerciales. Por otra parte, la exposición de los quistes de Globodera pallida y G. rostochiensis (nematodos del quiste de la patata) a las conidias de P. oxalicum, en ensayos in vitro o en microcosmos de suelo, reduce significativamente la capacidad de eclosión de los huevos. Para G. pallida esta reducción es mayor cuando se emplean exudados de raíz de patata del cv. 'Monalisa', que exudados de raíz del cv. 'Desirée'. No hay una reducción significativa en la tasa de eclosión con exudados de raíz de tomate del cv. 'San Pedro'. Para G. rostochiensis la reducción en la tasa de eclosión de los huevos se obtiene con exudados de la raíz de patata del cv. 'Desirée'. El tratamiento con P. oxalicum reduce también significativamente el número de quistes de G. pallida en macetas. Con el fin de optimizar la aplicación práctica de P. oxalicum cepa 212 como tratamiento biológico del suelo, es esencial entender cómo el entorno físico influye en la capacidad de colonización, crecimiento y supervivencia del mismo, así como el posible riesgo que puede suponer su aplicación sobre el resto de los microorganismos del ecosistema. Por ello en este segundo objetivo de esta tesis se estudia la interacción del ACB con el medio ambiente en el cual se aplica. Dentro de este objetivo se evalúa la INFLUENCIA DE LA TEMPERATURA, DISPONIBILIDAD DE AGUA Y PROPIEDADES FÍSICO-QUÍMICAS DE LOS SUELOS (POROSIDAD, TEXTURA, DENSIDAD...) SOBRE LA SUPERVIVENCIA Y EL CRECIMIENTO DE PO212 en condiciones controladas elaborando modelos que permitan predecir el impacto de cada factor ambiental en la supervivencia y crecimiento de P. oxalicum y conocer su capacidad para crecer y sobrevivir en diferentes ambientes. En las muestras de suelo se cuantifica: i) la supervivencia de Penicillium spp. usando el recuento del número de unidades formadoras de colonias en un medio de cultivo semi-selectivo y ii) el crecimiento (biomasa) de PO212 mediante PCR en tiempo real. En los resultados obtenidos se demuestra que P. oxalicum crece y sobrevive mejor en condiciones de sequía independientemente de la temperatura y del tipo de suelo. Si comparamos tipos de suelo P. oxalicum crece y sobrevive en mayor medida en suelos areno-arcillosos con un bajo contenido en materia orgánica, un mayor pH y una menor disponibilidad de fósforo y nitrógeno. La supervivencia y el crecimiento de P. oxalicum se correlaciona de forma negativa con la disponibilidad de agua y de forma positiva con el contenido de materia orgánica. Sólo la supervivencia se correlaciona también positivamente con el pH. Por otro lado se realizan ensayos en suelos de huertos comerciales con diferentes propiedades físico-químicas y diferentes condiciones ambientales para ESTUDIAR EL ESTABLECIMIENTO, SUPERVIVENCIA Y DISPERSIÓN VERTICAL Y MOVILIDAD HORIZONTAL DE PO212. P. oxalicum 212 puede persistir y sobrevivir en esos suelos al menos un año después de su liberación pero a niveles similares a los de otras especies de Penicillium indígenas presentes en los mismos suelos naturales. Además, P. oxalicum 212 muestra una dispersión vertical y movilidad horizontal muy limitada en los diferentes tipos de suelo evaluados. La introducción de P. oxalicum en un ambiente natural no sólo implica su actuación sobre el microorganismo diana, el patógeno, si no también sobre otros microorganismos indígenas. Para EVALUAR EL EFECTO DE LA APLICACIÓN DE P. oxalicum SOBRE LAS POBLACIONES FÚNGICAS INDIGENAS PRESENTES EN EL SUELO de dos huertos comerciales, se analizan mediante electroforesis en gradiente desnaturalizante de poliacrilamida (DGGE) muestras de dichos suelos a dos profundidades (5 y 10 cm) y a cuatro fechas desde la aplicación de P. oxalicum 212 (0, 75, 180 y 365 días). El análisis de la DGGE muestra que las diferencias entre las poblaciones fúngicas se deben significativamente a la fecha de muestreo y son independientes del tratamiento aplicado y de la profundidad a la que se tomen las muestras. Luego, la aplicación del ACB no afecta a la población fúngica de los dos suelos analizados. El análisis de las secuencias de la DGGE confirma los resultados anteriores y permiten identificar la presencia del ACB en los suelos. La presencia de P. oxalicum en el suelo se encuentra especialmente relacionada con factores ambientales como la humedad. Por tanto, podemos concluir que Penicillium oxalicum cepa 212 puede considerarse un óptimo Agente de Control Biológico (ACB), puesto que es ecológicamente competitivo, eficaz para combatir un amplio espectro de enfermedades y no supone un riesgo para el resto de microorganismos fúngicos no diana presentes en el lugar de aplicación. ABSTRACT Currently, reduction of active (EU) and the implementation of the new EU Directive 2009/128 which establishing the framework for action to achieve the sustainable use of chemical pesticides and preference of use of biological, physical and other non-chemical methods, forces to look for control methods less harmful to the environment. Biological control (CB) of plant diseases using biological control agents (BCA) is perceived as a safer alternative and with less environmental impact, either alone or as part of an integrated control strategy. The isolate 212 of Penicillium oxalicum (PO212) (ATCC 201888) was originally isolated from the soil mycoflora in Spain. P. oxalicum is a promising biological control agent for Fusarium wilt and other tomato diseases. Once identified and characterized the BCA, was developed a mass production method of conidia by solid-state fermentation. After determined the process of obtaining a formulated product of the BCA by drying of product by fluid-bed drying, it enables the preservation of the inoculum over a long period of time. Finally, some formulations of dried P. oxalicum conidia have been developed which contain one different additive that have improved their viability, stability and facilitated its handling and application. However, further work is needed to improve biocontrol efficacy. The first objective of this thesis has focused on the study of the interaction BCA- pathogen-host, to allow P.oxalicum to work in different pathosystems. The first point to be addressed in this objective is the development of new FORMULATIONS of BCA which increase their effectiveness against vascular wilt of tomato. PO212 conidial formulations were obtained by the joint addition of various additives (wetting agents, adhesives or stabilizers) at two different points of the production-drying process: i) to substrate in the fermentation bags before the production process, and (ii) to conidial paste obtained after production but before drying. Of the 22 new formulations developed and evaluated in tomato plants in greenhouse tests, six of them (FOR22 , FOR25 , FOR32 , FOR35 , FOR36 and FOR3) improved significantly (P = 0.05) the biocontrol efficacy against tomato wilt with respect to that obtained with dried P.oxalicum conidia without additives (CSPO) or the fungicide Bavistin. The formulations that improve the efficiency of dried conidia without additives are those containing as humectants sodium alginate in the fermentation bags, followed by those containing glycerol as a stabilizer in the fermentation bags, and methylcellulose and skimmed milk as adherents before drying. Moreover, control of vascular wilt of tomatoes by PO212 conidial formulations is related to the date of disease onset. Another way to further improve the effectiveness of biocontrol is to improve the active substance by SELECTION OF NEW STRAINS of P. oxalicum, which may have different levels of effectiveness. Of the 28 new strains of P. oxalicum tested in a culture chamber, only PO15 isolate shows the same effectiveness that PO212 (62-67 % of control) against tomato vascular wilt in cases of high disease pressure. Whereas in cases of low disease pressure all strains of P. oxalicum and its mixtures effective. Finally, we study extend the range of action of this BCA TO OTHER GUESTS AND OTHER PATHOGENS AND DIFFERENT DEGREES OF VIRULENCE. In efficacy trials of P. oxalicum against isolates of different aggressiveness of Verticillium spp. and Fusarium oxysporum f. sp. lycopersici in tomato plants in growth chambers, shows that the efficiency of PO212 is negatively correlated with the level of disease caused by F. oxysporum f. sp. lycopersici. There is not differential effect in reducing the incidence or severity depending on the virulence of isolates. However, PO212 cause a greater reduction of disease in plants inoculated with virulent isolates media of V. dahlia. PO212 efficacy was also higher against isolates of high and average virulence of F. oxysporum f. sp. melonis and F. oxysporum f. sp. niveum in melon and watermelon plants, respectively. In both hosts the optimum dose of the BCA application is 107 conidia PO212 g-1 soil, applied on seedlings 7 days before transplantation into the field. Moreover, the reapplication of PO212 (2-4 times) to the roots by irrigation into the field improve efficiency of biocontrol. The efficacy of PO212 is not limited to vascular pathogens as those mentioned above, but also other pathogens such as Oomycetes (Phytophthora cactorum) and nematodes (Globodera pallida and G. rostochiensis). PO212 significantly reduces symptoms (50 %) caused by P. cactorum in strawberry nursery plants after application of BCA by dipping the roots before transplanting to soil in commercial nurseries. Moreover, the exposure of G. pallida and G. rostochiensis cysts to the conidia of P. oxalicum, in in vitro assays or in soil microcosms significantly reduces hatchability of eggs. The reduction in the rate of G. pallida juveniles hatching was greatest when root diffusates from the `Monalisa´ potato cultivar were used, followed by root diffusates from the `Désirée´ potato cultivar. However, no significant reduction in the rate of G. pallida juveniles hatching was found when root diffusates from the ‘San Pedro” tomato cultivar were used. For G. rostochiensis reduction in the juveniles hatching is obtained from the root diffusates 'Desirée' potato cultivar. Treatment with P. oxalicum also significantly reduces the number of cysts of G. pallida in pots. In order to optimize the practical application of P. oxalicum strain 212 as a biological soil treatment, it is essential to understand how the physical environment influences the BCA colonization, survival and growth, and the possible risk that can cause its application on other microorganisms in the ecosystem of performance. Therefore, the second objective of this thesis is the interaction of the BCA with the environment in which it is applied. Within this objective is evaluated the INFLUENCE OF TEMPERATURE, WATER AVAILABILITY AND PHYSICAL-CHEMICAL PROPERTIES OF SOILS (POROSITY, TEXTURE, DENSITY...) ON SURVIVAL AND GROWTH OF PO212 under controlled conditions to develop models for predicting the environmental impact of each factor on survival and growth of P. oxalicum and to know their ability to grow and survive in different environments. Two parameters are evaluated in the soil samples: i) the survival of Penicillium spp. by counting the number of colony forming units in semi-selective medium and ii) growth (biomass) of PO212 by real-time PCR. P. oxalicum grows and survives better in drought conditions regardless of temperature and soil type. P. oxalicum grows and survives more in sandy loam soils with low organic matter content, higher pH and lower availability of phosphorus and nitrogen. Survival and growth of P. oxalicum negatively correlates with the availability of water and positively with the organic content. Only survival also correlated positively with pH. Moreover, trials are carried out into commercial orchards soils with different physic-chemical properties and different environmental conditions TO STUDY THE ESTABLISHMENT, SURVIVAL, VERTICAL DISPERSION AND HORIZONTAL SPREAD OF PO212. P. oxalicum 212 can persist and survive at very low levels in soil one year after its release. The size of the PO212 population after its release into the tested natural soils is similar to that of indigenous Penicillium spp. Furthermore, the vertical dispersion and horizontal spread of PO212 is limited in different soil types. The introduction of P. oxalicum in a natural environment not only involves their action on the target organism, the pathogen, but also on other indigenous microorganisms. TO ASSESS THE EFFECT OF P. oxalicum APPLICATION ON SOIL INDIGENOUS FUNGAL COMMUNITIES in two commercial orchards, soil samples are analyzed by Denaturing Gradient Gel Electrophoresis polyacrylamide (DGGE). Samples are taken from soil at two depths (5 and 10 cm) and four dates from the application of P. oxalicum 212 (0, 75, 180 and 365 days). DGGE analysis shows that differences are observed between sampling dates and are independent of the treatment of P. oxalicum applied and the depth. BCA application does not affect the fungal population of the two soil analyzed. Sequence analysis of the DGGE bands confirms previous findings and to identify the presence of BCA on soils. The presence of P. oxalicum in soil is especially related to environmental factors such as humidity. Therefore, we conclude that the 212 of strain Penicillium oxalicum can be considered an optimum BCA, since it is environmentally competitive and effective against a broad spectrum of diseases and does not have any negative effect on soil non-target fungi communities.

Modeling soil system: complexity under your feet

A clear statement in these lines textually cited (Byers et al., 1938) defines the framework of this special issue: “True soil is the product of the action of climate and living organism upon the parent material, as conditioned by the local relief. The length of time during which these forces are operative is of great importance in determining the character of the ultimate product. Drainage conditions are also important and are controlled by local relief, by the nature of the parent material or underlying rock strata, or by the amount of precipitation in relation to rate of percolation and runoff water. There are, therefore, five principal factors of soil formation: Parent material, climate, biological activity, relief and time. These soil forming factors are interdependent, each modifying the effectiveness of the others.” Due to these various processes associated to its formation and genesis soil dynamics reveals high complexity that creates several levels of structure using this term in a broad sense

Nonlinear and Scaling Processes in Hydrology and Soil Science

Hydrology is the study of the properties, distribution and effects of water on the Earth?s soil, rocks and atmosphere. It also encompasses the study of the hydrologic cycle of precipitation, runoff, infiltration, storage, and evaporation, including the physical, biological and chemical reaction of water with the earth and its relation to life?.

Community Structure in Soil Porous System

Diffusion controls the gaseous transport process in soils when advective transport is almost null. Knowledge of the soil structure and pore connectivity are critical issues to understand and modelling soil aeration, sequestration or emission of greenhouse gasses, volatilization of volatile organic chemicals among other phenomena. In the last decades these issues increased our attention as scientist have realize that soil is one of the most complex materials on the earth, within which many biological, physical and chemical processes that support life and affect climate change take place. A quantitative and explicit characterization of soil structure is difficult because of the complexity of the pore space. This is the main reason why most theoretical approaches to soil porosity are idealizations to simplify this system. In this work, we proposed a more realistic attempt to capture the complexity of the system developing a model that considers the size and location of pores in order to relate them into a network. In the model we interpret porous soils as heterogeneous networks where pores are represented by nodes, characterized by their size and spatial location, and the links representing flows between them. In this work we perform an analysis of the community structure of porous media of soils represented as networks. For different real soils samples, modelled as heterogeneous complex networks, spatial communities of pores have been detected depending on the values of the parameters of the porous soil model used. These types of models are named as Heterogeneous Preferential Attachment (HPA). Developing an exhaustive analysis of the model, analytical solutions are obtained for the degree densities and degree distribution of the pore networks generated by the model in the thermodynamic limit and shown that the networks exhibit similar properties to those observed in other complex networks. With the aim to study in more detail topological properties of these networks, the presence of soil pore community structures is studied. The detection of communities of pores, as groups densely connected with only sparser connections between groups, could contribute to understand the mechanisms of the diffusion phenomena in soils.

Community Structurein Soil Porous System.

Soil is well recognized as a highly complex system. The interaction and coupled physical, chemical, and biological processes and phenomena occurring in the soil environment at different spatial and temporal scales are the main reasons for such complexity. There is a need for appropriate methodologies to characterize soil porous systems with an interdisciplinary character. Four different real soil samples, presenting different textures, have been modeled as heterogeneous complex networks, applying a model known as the heterogeneous preferential attachment. An analytical study of the degree distributions in the soil model shows a multiscaling behavior in the connectivity degrees, leaving an empirically testable signature of heterogeneity in the topology of soil pore networks. We also show that the power-law scaling in the degree distribution is a robust trait of the soil model. Last, the detection of spatial pore communities, as densely connected groups with only sparser connections between them, has been studied for the first time in these soil networks. Our results show that the presence of these communities depends on the parameter values used to construct the network. These findings could contribute to understanding the mechanisms of the diffusion phenomena in soils, such as gas and water diffusion, development and dynamics of microorganisms, among others.

CO2 soil flux baseline at the technological development plant for CO2 injection at Hontomin (Burgos, Spain)

From the end of 2013 and during the following two years, 20 kt of CO2sc are planned to be injected in a saline reservoir (1500 m depth) at the Hontomín site (NE Spain). The target aquifers are Lower Jurassic limestone formations which are sealed by Lower Cretaceous clay units at the Hontomín site (NE Spain). The injection of CO2 is part of the activities committed in the Technology Development phase of the EC-funded OXYCFB300 project (European Energy Program for Recovery – EEPR, http://www.compostillaproject.eu), which include CO2 injection strategies, risk assessment, and testing and validating monitoring methodologies and techniques. Among the monitoring works, the project is intended to prove that present-day technology is able to monitor the evolution of injected CO2 in the reservoir and to detect potential leakage. One of the techniques is the measurement of CO2 flux at the soil–atmosphere interface, which includes campaigns before, during and after the injection operations. In this work soil CO2 flux measurements in the vicinity of oil borehole, drilled in the eighties and named H-1 to H-4, and injection and monitoring wells were performed using an accumulation chamber equipped with an IR sensor. Seven surveys were carried out from November 2009 to summer 2011. More than 4000 measurements were used to determine the baseline flux of CO2 and its seasonal variations. The measured values were low (from 5 to 13 g m−2 day−1) and few outliers were identified, mainly located close to the H-2 oil well. Nevertheless, these values cannot be associated to a deep source of CO2, being more likely related to biological processes, i.e. soil respiration. No anomalies were recognized close to the deep fault system (Ubierna Fault) detected by geophysical investigations. There, the CO2 flux is indeed as low as other measurement stations. CO2 fluxes appear to be controlled by the biological activity since the lowest values were recorded during autumn-winter seasons and they tend to increase in warm periods. Two reference CO2 flux values (UCL50 of 5 g m−2 d−1 for non-ploughed areas in autumn–winter seasons and 3.5 and 12 g m−2 d−1 for in ploughed and non-ploughed areas, respectively, in spring–summer time, and UCL99 of 26 g m−2 d−1 for autumn–winter in not-ploughed areas and 34 and 42 g m−2 d−1 for spring–summer in ploughed and not-ploughed areas, respectively) were calculated. Fluxes higher than these reference values could be indicative of possible leakage during the operational and post-closure stages of the storage project.

Morphological Functions to Quantify Three-Dimensional Tomograms of Macropore Structure in a Vineyard Soil with Two Different Management Regimes

Soil tomography and morphological functions built over Minkowski functionals were used to describe the impact on pore structure of two soil management practices in a Mediterranean vineyard. Soil structure controls important physical and biological processes in soil–plant–microbial systems. Those processes are dominated by the geometry of soil pore structure, and a correct model of this geometry is critical for understanding them. Soil tomography has been shown to provide rich three-dimensional digital information on soil pore geometry. Recently, mathematical morphological techniques have been proposed as powerful tools to analyze and quantify the geometrical features of porous media. Minkowski functionals and morphological functions built over Minkowski functionals provide computationally efficient means to measure four fundamental geometrical features of three-dimensional geometrical objects, that is, volume, boundary surface, mean boundary surface curvature, and connectivity. We used the threshold and the dilation and erosion of three-dimensional images to generate morphological functions and explore the evolution of Minkowski functionals as the threshold and as the degree of dilation and erosion changes. We analyzed the three-dimensional geometry of soil pore space with X-ray computed tomography (CT) of intact soil columns from a Spanish Mediterranean vineyard by using two different management practices (conventional tillage versus permanent cover crop of resident vegetation). Our results suggested that morphological functions built over Minkowski functionals provide promising tools to characterize soil macropore structure and that the evolution of morphological features with dilation and erosion is more informative as an indicator of structure than moving threshold for both soil managements studied.

Decoupling of soil nutrient cycles as a function of aridity in global drylands

The biogeochemical cycles of carbon (C), nitrogen (N) and phosphorus (P) are interlinked by primary production, respiration and decomposition in terrestrial ecosystems. It has been suggested that the C, N and P cycles could become uncoupled under rapid climate change because of the different degrees of control exerted on the supply of these elements by biological and geochemical processes. Climatic controls on biogeochemical cycles are particularly relevant in arid, semi-arid and dry sub-humid ecosystems (drylands) because their biological activity is mainly driven by water availability. The increase in aridity predicted for the twenty-first century in many drylands worldwide may therefore threaten the balance between these cycles, differentially affecting the availability of essential nutrients. Here we evaluate how aridity affects the balance between C, N and P in soils collected from 224 dryland sites from all continents except Antarctica. We find a negative effect of aridity on the concentration of soil organic C and total N, but a positive effect on the concentration of inorganic P. Aridity is negatively related to plant cover, which may favour the dominance of physical processes such as rock weathering, a major source of P to ecosystems, over biological processes that provide more C and N, such as litter decomposition. Our findings suggest that any predicted increase in aridity with climate change will probably reduce the concentrations of N and C in global drylands, but increase that of P. These changes would uncouple the C, N and P cycles in drylands and could negatively affect the provision of key services provided by these ecosystems.

Parallel sets and morphological measurements of CT images of soil pore structure in a vineyard

Important physical and biological processes in soil-plant-microbial systems are dominated by the geometry of soil pore space, and a correct model of this geometry is critical for understanding them. We analyze the geometry of soil pore space with the X-ray computed tomography (CT) of intact soil columns. We present here some preliminary results of our investigation on Minkowski functionals of parallel sets to characterize soil structure. We also show how the evolution of Minkowski morphological measurements of parallel sets may help to characterize the influence of conventional tillage and permanent cover crop of resident vegetation on soil structure in a Spanish Mediterranean vineyard.

Identification of pore spaces in 3D CT soil images using a PFCM partitional clustering

Recent advances in non-destructive imaging techniques, such as X-ray computed tomography (CT), make it possible to analyse pore space features from the direct visualisation from soil structures. A quantitative characterisation of the three-dimensional solid-pore architecture is important to understand soil mechanics, as they relate to the control of biological, chemical, and physical processes across scales. This analysis technique therefore offers an opportunity to better interpret soil strata, as new and relevant information can be obtained. In this work, we propose an approach to automatically identify the pore structure of a set of 200-2D images that represent slices of an original 3D CT image of a soil sample, which can be accomplished through non-linear enhancement of the pixel grey levels and an image segmentation based on a PFCM (Possibilistic Fuzzy C-Means) algorithm. Once the solids and pore spaces have been identified, the set of 200-2D images is then used to reconstruct an approximation of the soil sample by projecting only the pore spaces. This reconstruction shows the structure of the soil and its pores, which become more bounded, less bounded, or unbounded with changes in depth. If the soil sample image quality is sufficiently favourable in terms of contrast, noise and sharpness, the pore identification is less complicated, and the PFCM clustering algorithm can be used without additional processing; otherwise, images require pre-processing before using this algorithm. Promising results were obtained with four soil samples, the first of which was used to show the algorithm validity and the additional three were used to demonstrate the robustness of our proposal. The methodology we present here can better detect the solid soil and pore spaces on CT images, enabling the generation of better 2D?3D representations of pore structures from segmented 2D images.

Does the natural "microcosm" created by Tuber aestivum affect soil microarthropods? A new hypothesis based on Collembola in truffle culture

microarthropods play an important role in fungi dispersion, but little is still known about the interaction between truffle and soil microarthropods. The aim of this study was to investigate the ability of the truffle Tuber aestivum to modify soil biogeochemistry (i.e. create a zone of scarce vegetation around the host plant, called a burn or brûlé) and to highlight the effects of the brûlé on the soil fauna community. We compared soil microarthropod communities found in the soil inside versus outside the T. aestivum brûlé with the chemistry of soil collected inside versus outside the brûlé. The study was carried out in three Mediterranean areas, two in Italy and one in Spain. The results confirmed the ability of T. aestivum to modify soil biogeochemistry in the brûlé: pH was higher and total organic carbon tended to be lower inside the brûlé compared to outside. Soil fauna communities showed some interesting differences. Some groups, such as Symphyla and Pauropoda, adapted well to the soil; some Collembolan families, and biodiversity and soil quality indices were generally higher outside the brûlé. Folsomia sp. showed higher abundance in the soil of the brûlé compared to outside. The results suggest that some Collembola groups may be attracted by the fungal metabolites produced by T. aestivum, while other Collembola and other microarthropods may find an unfavourable environment in the soil of the brûlé. The next steps will be to confirm this hypothesis and to extend the study to other keys groups such as nematodes and earthworms and to link fluctuations of soil communities with the biological phases of truffle growth.

Nematodes as indicators of the effect of soil fumigants on soil functioning

Debido al futuro incierto de la mayor parte de los fumigantes edáficos usados actualmente en la Unión Europea, que pueden implicar riesgos para la salud humana/animal y el medio ambiente, es necesario desarrollar programas de manejo integrado para el control de plagas de cultivos. Estos programas se incluyen como obligatorios en el Reglamento (EC) No. 1107/2009. De acuerdo con este Reglamento, es obligatoria la evaluación del riesgo asociado al uso de productos fitosanitarios sobre los organismos edáficos no diana y sus funciones, además de llevar a cabo ensayos con diferentes especies indicadoras para obtener datos de toxicidad que puedan ser usados posteriormente en la evaluación de riesgo. Sin embargo, la baja representatividad de algunas de estas especies indicadoras en el área Mediterránea supone una gran limitación. En esta situación, el Panel Científico de Productos Fitosanitarios y sus Residuos de la Autoridad Europea en Seguridad Alimentaria (EFSA), ha señalado la necesidad de modificar los datos ecotoxicológicos requeridos para evaluar los efectos adversos de los productos fitosanitarios de una manera más integrada, incluyendo criterios funcionales y estructurales mediante organismos como bacterias, hongos, protozoos y nematodos. De este modo, la EFSA ha recomendado el uso de los nematodos en la evaluación de la funcionalidad y estructura del suelo. Los nematodos están globalmente distribuidos y son morfológicamente diversos; esto junto con su gran abundancia y diversidad de respuestas a las perturbaciones edáficas, los convierte en indicadores adecuados del estado del suelo. Puesto que los nematodos interaccionan con muchos otros organismos que participan en diferentes eslabones de la red trófica edáfica, jugando papeles importantes en procesos edáficos esenciales en los agroescosistemas, la diversidad de nematodos es, a menudo, usada como indicador biológico de los efectos de las prácticas agrícolas en el estado del suelo. En los últimos años, diferentes índices basados en la comunidad nematológica han facilitado la interpretación de datos complejos sobre la ecología del suelo. Los índices de la red trófica edáfica, basados en la abundancia de grupos funcionales definidos como grupos C-P y grupos tróficos, permiten la evaluación de la funcionalidad de la red trófica edáfica. Por otra parte, la dificultad en la identificación taxonómica de nematodos para explicar su uso limitado como indicadores ecológicos, es ampliamente discutida, y existe cierta controversia en cuanto a la eficacia de los diferentes métodos de identificación de nematodos. Se argumenta que la identificación morfológica es difícil y puede llevar mucho tiempo debido a la falta de expertos especializados, y se afirma que las técnicas moleculares pueden resolver algunas limitaciones de las técnicas morfológicas como la identificación de juveniles. Sin embargo, los métodos de identificación molecular tienen también limitaciones; la mayoría de las bases de datos de secuencias de ADN están fuertemente orientadas hacia los nematodos fitoparásitos, los cuales representan sólo una parte de la comunidad edáfica de nematodos, mientras que hay poca información disponible de nematodos de vida libre a pesar de representar la mayoría de los nematodos edáficos. Este trabajo se centra en el estudio de los efectos de fumigantes edáficos en la funcionalidad del suelo a través del uso de diferentes indicadores basados en la comunidad de nematodos, como los índices de la red trófica, índices de diversidad, abundancia de los taxones más relevantes etc. También se han analizado otros indicadores funcionales relacionados con la supresividad edáfica, el ciclo de nutrientes o la actividad de la microfauna del suelo. En el capítulo 1, la diversidad de nematodos estudiada en una explotación comercial de fresa y sus alrededores durante dos campañas consecutivas en el suroeste español, fue baja en los suelos fumigados con fumigantes químicos ambas campañas y, aunque se observó una recuperación a lo largo de la campaña en la zona tratada, los suelos fumigados mostraron una condición perturbada permanente. La comunidad de nematodos estuvo más asociada al ciclo de nutrientes en la zona sin cultivar que en los suelos cultivados, y se observó poca relación entre la biomasa de las plantas y la estructura de la comunidad de nematodos. Los surcos sin tratar dentro de la zona de cultivo funcionaron como reservorio tanto de nematodos fitoparásitos como beneficiosos; sin embargo estas diferencias entre los surcos y los lomos de cultivo no fueron suficientes para mantener la supresividad edáfica en los surcos. Los suelos tratados fueron menos supresivos que los suelos sin tratar, y se observaron correlaciones positivas entre la supresividad edáfica y la estructura de la red trófica edáfica y la diversidad de nematodos. En el capítulo 2, se evaluaron los efectos de dos pesticidas orgánicos con efecto nematicida y dos nematicidas convencionales sobre las propiedades físico químicas del suelo, la diversidad de nematodos y la biomasa de las plantas en condiciones experimentales en dos tipos de suelo: suelos agrícolas poco diversos y suelos provenientes de una zona de vegetación natural muy diversos. El mayor efecto se observó en el tratamiento con neem, el cual indujo un gran incremento en el número de dauerlarvas en los suelos pobres en nutrientes, mientras que el mismo tratamiento indujo un incremento de poblaciones de nematodos bacterívoros, más estables y menos oportunistas, en los suelos del pinar ricos en materia orgánica. En el capítulo 3, se comparó la eficacia de métodos moleculares (TRFLP, Terminal Restriction Fragment Length Polymorphism) y morfológicos (microscopía de alta resolución) para la identificación de diferentes comunidades denematodos de España e Irlanda. Se compararon estadísticamente las diferencias y similitudes en la diversidad de nematodos, otros indicadores ecológicos y de la red trófica edáfica. Las identificaciones mediante el uso de TRFLP sólo detectó un porcentaje de los taxones presentes en las muestras de suelo identificadas morfológicamente, y los nematodos omnívoros y predadores no fueron detectados molecularmente en nuestro estudio. Los índices calculados en base a los nematodos micróboros mostraron más similitud cuando se identificaron morfológica y molecularmente que los índices basados en grupos tróficos más altos. Nuestros resultados muestran que, al menos con la técnica usada en este estudio, la identificación morfológica de nematodos es una herramienta fiable y más precisa que la identificación molecular, puesto que en general se obtiene una mayor resolución en la identificación de nematodos. En el capítulo 4, se estudiaron también los efectos de los nematicidas químicos sobre la comunidad de nematodos y la biomasa de las plantas en condiciones experimentales de campo, donde se aplicaron en una rotación de cultivo judía-col durante un ciclo de cultivo. Se aplicaron dos tipos de enmiendas orgánicas con el objetivo de mitigar el efecto negativo de los productos fitosanitarios sobre la diversidad edáfica. El efecto de los nematicidas sobre las propiedades del suelo y sobre la comunidad de nematodos fue más agudo que el efecto de las enmiendas. La incorporación de los restos de cosecha al final del ciclo de cultivo de la judía tuvo un gran efecto sobre la comunidad de nematodos, y aunque el número total de nematodos incrementó al final del experimento, se observó una condición perturbada permanente de la red trófica edáfica a lo largo del experimento. ABSTRACT Due to the uncertain future of the soil fumigants most commonly used in the EU, that might involve risks for human/animal health and the environment, there is a need to develop new integrated pest management programs, included as mandatory in the Regulation (EC) No. 1107/2009, to control crop diseases. According to this Regulation, evaluating the risk associated to the use of the plant production products (PPP) on non-target soil fauna and their function, and developing assays with different indicator species to obtain toxicity data to be used in the risk evaluation is mandatory. However, the low representativeness of some of these indicator species in the Mediterranean area is a relevant limitation. In this situation, the Scientific Panel of Plant Protection Products and their Residues of the European Food Safety Authority (EFSA) has pointed out the necessity of modifying the ecotoxicological data set required to evaluate non-target effects of PPP in a more integrated way, including structural and functional endpoints with organism such as bacteria, fungi, protists and nematodes. Thus, EFSA has recommended the use of nematodes in the assessment of the functional and structural features of the soil. Nematodes are globally distributed and morphologically diverse, and due to their high abundance and diversity of responses to soil disturbance, they are suitable indicators of the soil condition. Since nematodes interact with many other organisms as participants in several links of the soil food web, playing important roles in essential soil processes in agroecosystems, nematode diversity is often used as a biological indicator of the effects of agricultural practices on soil condition. In the last years, various indices based on soil nematode assemblages, have facilitated the interpretation of complex soil ecological data. Soil food web indices based on the abundances of functional guilds defined by C-P groups and trophic groups, permit evaluating soil food web functioning. On the other hand, the difficulty of nematode taxonomical identification is commonly argued to explain their limited used as ecological indicators, and there is a certain controversy in terms of the efficacy of various nematode identification methods. It is argued that the morphological identification is difficult and time consuming due to the lack of specialist knowledge, and it is claimed that molecular techniques can solve some limitations of morphological techniques such as the identification of juveniles. Nevertheless, molecular identification methods are limited too, since most of the DNA-based databases are strongly oriented towards plant-parasitic nematodes that represent only a fraction of the soil nematode community, while there is little information available on free-living nematodes, which represent most soil nematodes. This work focuses on the study of the effects of soil fumigants on soil functioning through the use of different indicators based on soil nematode community as soil food web indices, diversity indices, the abundance of more relevant taxa etc. Other functional indicators related to soil suppressiveness, nutrient cycling, or the activity of soil microfauna have been also studied. In chapter 1, nematode diversity assessed in a commercial strawberry farm and its surroundings for two consecutive growing seasons in southern Spain, was low in fumigated soils with chemical pesticides throughout both seasons and, although yearly recovery occurred within the treated fields, fumigated soils showed a permanent perturbed condition. The nematode community was more closely associated to nutrient cycling in the non-cropped than in the cropped soils, and the link between plant biomass and nematode community structure was weak. Non-treated furrows within the treated fields were a reservoir of both beneficial and plant-parasitic nematodes, but such difference between furrows and beds was not enough to maintain more suppressive soil assemblages in the furrows. Treated soils were less suppressive than unmanaged soils, and there was a positive and significant correlation between soil suppressiveness and soil food web structure and diversity. In chapter 2, the effects of two organic pesticides with nematicide effect and two chemical nematicides on soil physicalchemical properties, soil nematode diversity and plant biomass in experimental conditions were assessed in two types of soils: low diversity soils from an agricultural farm, and high diversity soils from a natural vegetation area. The larger effect was observed on the neem treatment, which induced a large boost of dauer juveniles in the nutrient-depleted soil, while the same treatment induced the increase of more stable, less opportunistic, populations of generalist bacterivore nematodes in the pine forest soil, rich in organic matter. In chapter 3, comparison of the efficiency of molecular (TRFLP, Terminal Restriction Fragment Length Polymorphism) and morphological (microscopy at high magnification) identification methods was carried out in different nematode communities from five sites of different land uses in Spain and Ireland. Differences and similarities on nematode diversity and other ecological and soil food web indices assessed by both methods, were statistically compared. Molecular identification with TRFLP only detected a percentage of the taxa present in the soil samples identified morphologically, and omnivores and predators were not detected molecularly in our study. Indices involving microbial feeding nematodes were more similar between identification methods than indices involving higher trophic links. Our results show that, at least with the technique used in this study, identifying nematodes morphologically is a reliable and more precise identification tool than molecular identification, since a higher taxonomic resolution is in general obtained compared to TRFLP. In chapter 4, the effect of chemical nematicides on nematode community descriptors and plant biomass was also studied in field conditions in an experimental area in which dazomet and dimethyl disulfide was applied in a bean-cabbage rotation system for a single season. Organic amendments were incorporated into the soil with the aim of mitigate the negative effect of the pesticides on soil diversity. The effect of the nematicides was much more noticeable than the effect of the amendments on soil properties and nematode community descriptors. The incorporation of bean crop residues into the soil at the end of bean crop cycle affected soil nematode community descriptors to a great extent, and although total number of nematodes increased at the end of the experiment, a permanent perturbed soil food web condition was observed along the experiment.

Geometrical characterization of undisturbed soil samples using X-ray computed tomography image analysis. Effect of soil management on soil structure

El estudio de la estructura del suelo es de vital importancia en diferentes campos de la ciencia y la tecnología. La estructura del suelo controla procesos físicos y biológicos importantes en los sistemas suelo-planta-microorganismos. Estos procesos están dominados por la geometría de la estructura del suelo, y una caracterización cuantitativa de la heterogeneidad de la geometría del espacio poroso es beneficiosa para la predicción de propiedades físicas del suelo. La tecnología de la tomografía computerizada de rayos-X (CT) nos permite obtener imágenes digitales tridimensionales del interior de una muestra de suelo, proporcionando información de la geometría de los poros del suelo y permitiendo el estudio de los poros sin destruir las muestras. Las técnicas de la geometría fractal y de la morfología matemática se han propuesto como una poderosa herramienta para analizar y cuantificar características geométricas. Las dimensiones fractales del espacio poroso, de la interfaz poro-sólido y de la distribución de tamaños de poros son indicadores de la complejidad de la estructura del suelo. Los funcionales de Minkowski y las funciones morfológicas proporcionan medios para medir características geométricas fundamentales de los objetos geométricos tridimensionales. Esto es, volumen, superficie, curvatura media de la superficie y conectividad. Las características del suelo como la distribución de tamaños de poros, el volumen del espacio poroso o la superficie poro-solido pueden ser alteradas por diferentes practicas de manejo de suelo. En este trabajo analizamos imágenes tomográficas de muestras de suelo de dos zonas cercanas con practicas de manejo diferentes. Obtenemos un conjunto de medidas geométricas, para evaluar y cuantificar posibles diferencias que el laboreo pueda haber causado en el suelo. ABSTRACT The study of soil structure is of vital importance in different fields of science and technology. Soil structure controls important physical and biological processes in soil-plant-microbial systems. Those processes are dominated by the geometry of soil pore structure, and a quantitative characterization of the spatial heterogeneity of the pore space geometry is beneficial for prediction of soil physical properties. The technology of X-ray computed tomography (CT) allows us to obtain three-dimensional digital images of the inside of a soil sample providing information on soil pore geometry and enabling the study of the pores without disturbing the samples. Fractal geometry and mathematical morphological techniques have been proposed as powerful tools to analyze and quantify geometrical features. Fractal dimensions of pore space, pore-solid interface and pore size distribution are indicators of soil structure complexity. Minkowski functionals and morphological functions provide means to measure fundamental geometrical features of three-dimensional geometrical objects, that is, volume, boundary surface, mean boundary surface curvature, and connectivity. Soil features such as pore-size distribution, pore space volume or pore-solid surface can be altered by different soil management practices. In this work we analyze CT images of soil samples from two nearby areas with contrasting management practices. We performed a set of geometrical measures, some of them from mathematical morphology, to assess and quantify any possible difference that tillage may have caused on the soil.

Effects of biochar prepared from organic waste on soil properties

Biochar is a carbon-rich solid obtained by the thermal decomposition of organic matter under a limited supply of oxygen and at relatively low temperatures. Biochar can be prepared from the pyrolysis of different organic feed- stocks, such as wood and biomass crops, agricultural by-products, different types of waste or paper industry waste materials . The pyrolysis procedure of waste, i.e. sewage sludge, has mainly two advantages, firstly, it removes pathogens from waste and, secondly, biochar can reduce the leaching of heavy metals present in raw sewage sludge. This trend of the use of waste material as feedstocks to the preparation of biochar is increasing in the last years due to industrial development and economic growth imply an increase in waste generation. The application of biochar may have positive effects on soil physical properties as water holding capacity and structure or on soil biological activity and soil quality. Also, biochar can be used to remove water pollutants and can be used in multiple ways in soil remediation due to its adsorption of pesticides or metals. Also, biochar contribute to carbon sequestration due to carbon stability of biochar materials. The objective of this presentation is to review the positive effects of the biochar prepared from organic waste on soil properties.