Low vertical transfer rates of carbon inferred from radiocarbon analysis in an Amazon Podzol

Hydromorphic Podzol soils in the Amazon Basin generally support low-stature forests with some of the lowest amounts of aboveground net primary production (NPP) in the region. However, they can also exhibit large values of belowground NPP that can contribute significantly to the total annual inputs of organic matter into the soil. These hydromorphic Podzol soils also exhibit a horizon rich in organic matter at around 1?2m depth, presumably as a result of eluviation of dissolved organic matter and sesquioxides of Fe and Al. Therefore, it is likely that these ecosystems store large quantities of carbon by (1) large amounts of C inputs to soils dominated by their high levels of fine-root production, (2) stabilization of organic matter in an illuviation horizon due to significant vertical transfers of C. To assess these ideas we studied soil carbon dynamics using radiocarbon in two adjacent Amazon forests growing on contrasting soils: a hydromorphic Podzol and a well-drained Alisol supporting a high-stature terra firme forest. Our measurements showed similar concentrations of C and radiocarbon in the litter layer and the first 5 cm of the mineral soil for both sites. This result is consistent with the idea that the hydromorphic Podzol soil has similar soil C storage and cycling rates compared to the well-drained Alisol that supports a more opulent vegetation. However, we found important differences in carbon dynamics and transfers along the vertical profile. At both soils, we found similar radiocarbon concentrations in the subsoil, but the carbon released after incubating soil samples presented radiocarbon concentrations of recent origin in the Alisol, but not in the Podzol. There were no indications of incorporation of C fixed after 1950 in the illuvial horizon of the Podzol. With the aid of a simulation model, we predicted that only a minor fraction (1.7 %) of the labile carbon decomposed in the topsoil is transferred to the subsoil of the Podzol, while this proportional transfer is about 30% in the Alisol. Furthermore, our estimates were 8 times lower than previous estimations of vertical C transfers in Amazon Podzols, and question the validity of these previous estimations for all Podzols within the Amazon Basin. Our results also challenge our previous ideas about the genesis of these particular soils and suggest that either they are not true Podzols or the podzolization processes had already stopped.

Localización de reflectores mediante la utilización de la teoría de rayos a nivel dinámico

A partir de los años 60, comienza un desarrollo importante de los métodos que utilizan las características de reflexión del medio para la determinación de la estructura del subsuelo. Se han desarrollado técnicas muy precisas en el campo de la detección, fundamentalmente de recursos energéticos, pero aplicadas únicamente a nivel cinemática. Se intenta en este trabajo mostrar la posibilidad de utilizar la teoría de rayos a un segundo nivel, dinámico, para extraer más información del medio en menos tiempo, y, por lo tanto, con menor costo. Se ha utilizado el método de los elementos discretos triangulares = Since the sixties an important developmen of the methods which use the characteristics of environment reflexion for the determination of subsoil structure has taken place. Some very accurate technics have been developed in the detection field, principally energetic resources technics, but they have been only applied to a kinematic level. In this work we try to show the possibility of using ray theory in a second level: dinamic level, to get more information about the environment in less time, and so with less cost. The method of triangular discret elements has been used.

Sismicidad inducida por la manipulación del subsuelo

Los terremotos inducidos por la inyección de gas realizadas en la plataforma continental del golfo de Valencia, proyecto El Castor, en septiembre-octubre 2013, han creado cierta alarma social en las poblaciones costeras próximas. Esto, que es novedoso en España, ha ocurrido con cierta frecuencia en otras áreas pobladas en distintos países y por causa de varios tipos de manipulación del subsuelo. Este artículo intenta ilustrar el problema de la sismicidad inducida por la actividad del hombre. Según se describe en el texto, la sismicidad inducida tiene unos límites, máximo terremoto inducido, que pueden ser investigados en cada caso. De esa manera, se pueden establecer protocolos de actuación que impidan que dichas actividades causen daños materiales en las localidades próximas. Earthquakes induced by the gas injection in the continental platform, of the golf of Valencia, Castor Project, last September-October 2013, has motivated some social alarm within the nearby coastal population. That, which is new for Spain, has happened with some frequency at some other populated areas, in different countries and due to various types of subsoil manipulations. This article tries to illustrate the induced seismicity problem due to human activities. As it is described in the text, the induced seismicity has some limits (maximum induced earthquake) that can be investigated for each particular case. By this way, protocols of operation can be established to avoid that theses activities might cause material damage to local population.

Paisajes de la sal en Andalucía

Los paisajes protagonistas de esta investigación han sido creados gracias a la actividad de las salinas, explotaciones “donde se beneficia la sal de las aguas del mar o de ciertos manantiales, cuando se ha evaporado el agua.” (RAE). Son lugares de características únicas, tanto por sus valores naturales y medioambientales, como por los valores culturales, patrimoniales, históricos, sociales e identitarios, “resultado de la acción e interacción de factores naturales y humanos en el territorio” (CEP, 2000). Existen salinas en muchos lugares del mundo, pero es en la Península Ibérica donde se encuentra la mayor concentración de estas explotaciones en toda Europa y, por consiguiente, de los singulares paisajes asociados y generados por ellas. Es también la única región europea donde existen salinas de interior que utilizan métodos de evaporación para la obtención de sal: las energías y circunstancias naturales aprovechadas en ellas, sol, viento, gravedad y humedad relativa, propician la evaporación del agua salada, una de las estrategias fundamentales para su funcionamiento. Esta circunstancia determina su posición geográfica en el territorio y su dependencia de los ciclos climáticos estacionales, del régimen hidrológico, la estructura geológica del subsuelo, la geomorfología y la acción humana para potenciar la eficiencia de los procesos productivos, creando para ello un extenso e interesante patrimonio natural y cultural en torno a ellas. Por tanto, son también paisajes culturales, resultado de un proceso artesanal de producción y comercialización de la sal, que se articula a través de la construcción de una serie de instalaciones preindustriales diseminadas y conectadas en puntos estratégicos del territorio costero e interior. La presente tesis aborda la grave situación a la que se enfrentan en la actualidad los paisajes ibéricos de la sal, concretamente los ubicados en la Comunidad Autónoma de Andalucía, que están sufriendo un ávido proceso de abandono y desaparición desde mediados del s. XX, con la consiguiente pérdida para la sociedad de este valioso patrimonio cultural y natural, que se ha ido construyendo durante siglos, prácticamente desde el inicio de la humanidad. De las diversas tipologías de salinas que existen, se han seleccionado las explotaciones, tanto marítimas como de interior, que utilizan o han utilizado en su origen técnicas de explotación artesanal basadas en la evaporación. El interés de esta acotación tipológica se ha basado en las relaciones de dependencia que estas explotaciones de sal establecen con el entorno físico y climático donde se ubican para poder existir y funcionar. El objetivo principal de esta investigación ha perseguido el establecimiento y definición de un marco territorial, global e integrador, para los paisajes culturales salineros andaluces, a través de la observación directa realizada durante el trabajo de campo, el análisis de textos, imágenes, documentos, gráficos, palabras y entrevistas abiertas. Lo anterior ha permitido identificar, clasificar, analizar y valorar sus principales características y su evolución en el tiempo, identificando las causas del deterioro y desaparición del patrimonio salinero, evaluando la efectividad de las iniciativas, públicas y/o privadas, y de las figuras de protección, así como analizar las relaciones que establecen con su entorno próximo, con los núcleos de población y habitantes a los que sirven, la red de carreteas y caminos que las conectan y los ríos y mares que las proveen de materia prima. Finalmente, se ha establecido una sistemática integral de análisis, con el fin de poder actuar, a partir del conocimiento, a favor de la gestión, salvaguarda y pervivencia de los excepcionales valores culturales y naturales, que definen el carácter e identidad de estos singulares paisajes. ----------------------ABSTRACT----------------- The landscapes of this research have been created by the activity of saltworks, sites “where salt from sea water or certain springs is obtained, when water evaporates.” (RAE). They are places with unique characteristics, because of their natural and environmental values, as well as their cultural, historic and social values, their heritage and identity, “the result of the action and interaction of natural and human factors on the territory” (European Landscape Convention, 2000). There are many saltworks in many places around the world, but it is in the Iberian Peninsula where we find the highest concentration of salt industries within Europe and, therefore, the particular landscapes associated and created by them. It is as well the only European region where we can find inland saltworks with evaporation methods to obtain salt: the energies and natural circumstances used in them are sun, wind, gravity and relative humidity, favouring salt water evaporation, one of the main strategies of their functioning. This circumstance determines their geographic position in the territory and its dependence on seasonal climatic cycles, hydrological regimes, geological subsoil structure, geomorphology and human action to strengthen productive processes efficiency, creating an extensive and interesting natural and cultural heritage around them. Therefore, they are also cultural landscapes, result of a traditional salt production process and marketing, organized through the construction of certain preindustrial buildings scattered and connected in strategic inland and seaside spots. This thesis deals with the plight today’s salt landscapes are facing, particularly those within the Andalucian Region, since the middle of the 20th century undergoing an avid process of abandonment and disappearance, meaning a great loss for society of a cultural and natural heritage constructed along centuries, almost since the beginning of mankind. Among the diverse typologies of saltworks, the selection made consists on those inland and seaside ones, which use or have originally used traditional production techniques based on evaporation. The interest in this particular saltwork typology is based on the dependency relationships these industries establish with the environment and climate where they are located, in order to be able to exist and function. The main goal of this research has pursued to establish and define a global and inclusive territorial framework for Andalucian cultural saltworks landscapes, through direct observation carried out during fieldwork, analysis of texts, images, documents, graphs, words and open interviews. All of it has allowed to identify, classify, analyze and evaluate their main characteristics and evolution over time, identifying the causes of deterioration and disappearance of the saltworks heritage, assessing the effectiveness of public and private initiatives, and protection projects, as well as analyzing the relationships with their surroundings, population centers and residents they serve, road networks connecting them and rivers and seas supplying the raw material. Finally, a comprehensive analysis systematic has been established, in order to be able to take action, with knowledge as starting point, for the management, preservation and survival of the unique cultural and natural values that define the character and identity of these singular landscapes.

Paisajes de la sal en Andalucía

Los paisajes protagonistas de esta investigación han sido creados gracias a la actividad de las salinas, explotaciones “donde se beneficia la sal de las aguas del mar o de ciertos manantiales, cuando se ha evaporado el agua.” (RAE). Son lugares de características únicas, tanto por sus valores naturales y medioambientales, como por los valores culturales, patrimoniales, históricos, sociales e identitarios, “resultado de la acción e interacción de factores naturales y humanos en el territorio” (CEP, 2000). Existen salinas en muchos lugares del mundo, pero es en la Península Ibérica donde se encuentra la mayor concentración de estas explotaciones en toda Europa y, por consiguiente, de los singulares paisajes asociados y generados por ellas. Es también la única región europea donde existen salinas de interior que utilizan métodos de evaporación para la obtención de sal: las energías y circunstancias naturales aprovechadas en ellas, sol, viento, gravedad y humedad relativa, propician la evaporación del agua salada, una de las estrategias fundamentales para su funcionamiento. Esta circunstancia determina su posición geográfica en el territorio y su dependencia de los ciclos climáticos estacionales, del régimen hidrológico, la estructura geológica del subsuelo, la geomorfología y la acción humana para potenciar la eficiencia de los procesos productivos, creando para ello un extenso e interesante patrimonio natural y cultural en torno a ellas. Por tanto, son también paisajes culturales, resultado de un proceso artesanal de producción y comercialización de la sal, que se articula a través de la construcción de una serie de instalaciones preindustriales diseminadas y conectadas en puntos estratégicos del territorio costero e interior. La presente tesis aborda la grave situación a la que se enfrentan en la actualidad los paisajes ibéricos de la sal, concretamente los ubicados en la Comunidad Autónoma de Andalucía, que están sufriendo un ávido proceso de abandono y desaparición desde mediados del s. XX, con la consiguiente pérdida para la sociedad de este valioso patrimonio cultural y natural, que se ha ido construyendo durante siglos, prácticamente desde el inicio de la humanidad. De las diversas tipologías de salinas que existen, se han seleccionado las explotaciones, tanto marítimas como de interior, que utilizan o han utilizado en su origen técnicas de explotación artesanal basadas en la evaporación. El interés de esta acotación tipológica se ha basado en las relaciones de dependencia que estas explotaciones de sal establecen con el entorno físico y climático donde se ubican para poder existir y funcionar. El objetivo principal de esta investigación ha perseguido el establecimiento y definición de un marco territorial, global e integrador, para los paisajes culturales salineros andaluces, a través de la observación directa realizada durante el trabajo de campo, el análisis de textos, imágenes, documentos, gráficos, palabras y entrevistas abiertas. Lo anterior ha permitido identificar, clasificar, analizar y valorar sus principales características y su evolución en el tiempo, identificando las causas del deterioro y desaparición del patrimonio salinero, evaluando la efectividad de las iniciativas, públicas y/o privadas, y de las figuras de protección, así como analizar las relaciones que establecen con su entorno próximo, con los núcleos de población y habitantes a los que sirven, la red de carreteas y caminos que las conectan y los ríos y mares que las proveen de materia prima. Finalmente, se ha establecido una sistemática integral de análisis, con el fin de poder actuar, a partir del conocimiento, a favor de la gestión, salvaguarda y pervivencia de los excepcionales valores culturales y naturales, que definen el carácter e identidad de estos singulares paisajes. ----------------------ABSTRACT----------------- The landscapes of this research have been created by the activity of saltworks, sites “where salt from sea water or certain springs is obtained, when water evaporates.” (RAE). They are places with unique characteristics, because of their natural and environmental values, as well as their cultural, historic and social values, their heritage and identity, “the result of the action and interaction of natural and human factors on the territory” (European Landscape Convention, 2000). There are many saltworks in many places around the world, but it is in the Iberian Peninsula where we find the highest concentration of salt industries within Europe and, therefore, the particular landscapes associated and created by them. It is as well the only European region where we can find inland saltworks with evaporation methods to obtain salt: the energies and natural circumstances used in them are sun, wind, gravity and relative humidity, favouring salt water evaporation, one of the main strategies of their functioning. This circumstance determines their geographic position in the territory and its dependence on seasonal climatic cycles, hydrological regimes, geological subsoil structure, geomorphology and human action to strengthen productive processes efficiency, creating an extensive and interesting natural and cultural heritage around them. Therefore, they are also cultural landscapes, result of a traditional salt production process and marketing, organized through the construction of certain preindustrial buildings scattered and connected in strategic inland and seaside spots. This thesis deals with the plight today’s salt landscapes are facing, particularly those within the Andalucian Region, since the middle of the 20th century undergoing an avid process of abandonment and disappearance, meaning a great loss for society of a cultural and natural heritage constructed along centuries, almost since the beginning of mankind. Among the diverse typologies of saltworks, the selection made consists on those inland and seaside ones, which use or have originally used traditional production techniques based on evaporation. The interest in this particular saltwork typology is based on the dependency relationships these industries establish with the environment and climate where they are located, in order to be able to exist and function. The main goal of this research has pursued to establish and define a global and inclusive territorial framework for Andalucian cultural saltworks landscapes, through direct observation carried out during fieldwork, analysis of texts, images, documents, graphs, words and open interviews. All of it has allowed to identify, classify, analyze and evaluate their main characteristics and evolution over time, identifying the causes of deterioration and disappearance of the saltworks heritage, assessing the effectiveness of public and private initiatives, and protection projects, as well as analyzing the relationships with their surroundings, population centers and residents they serve, road networks connecting them and rivers and seas supplying the raw material. Finally, a comprehensive analysis systematic has been established, in order to be able to take action, with knowledge as starting point, for the management, preservation and survival of the unique cultural and natural values that define the character and identity of these singular landscapes.

Determinación de la amplificación sísmica local en el Campus Sur UPM mediante la técnica de sismología de microtremores ReMi.

En el Campus Sur de la Universidad Politécnica de Madrid se ha llevado a cabo un proyecto para obtener una caracterización del subsuelo mediante ensayos ReMi, en colaboración con el departamento de Geofísica del Instituto Geográfico Nacional. La técnica ReMi (Refraction Microtremor) permite, mediante ensayos geofísicos realizados localmente sobre el terreno,obtener los parámetros físicos del mismo, que resultan de especial interés en el ámbito de la ingeniería civil. Esta técnica se caracteriza por englobarse dentro de la sísmica pasiva, muy empleada en prospección geofísica y basada en la obtención del modelo subyacente de distribución de velocidades de propagación de la onda S en función de la profundidad, con la ventaja de aprovechar el ruido sísmico ambiental como fuente de energía. Fue desarrollada en el Laboratorio Sismológico de Nevada (EEUU) por Louie (2001), con el objetivo de presentar una técnica innovadora en la obtención de las velocidades de propagación de manera experimental. Presenta ciertas ventajas, como la observación directa de la dispersión de ondas superficiales,que da un buen resultado de la velocidad de onda S, siendo un método no invasivo, de bajo coste y buena resolución, aplicable en entornos urbanos o sensibles en los que tanto otras técnicas sismológicas como otras variedades de prospección presentan dificultades. La velocidad de propagación de la onda S en los 30 primeros metros VS30, es ampliamente reconocida como un parámetro equivalente válido para caracterizar geotécnicamente el subsuelo y se halla matemáticamente relacionada con la velocidad de propagación de las ondas superficiales a observar mediante la técnica ReMi. Su observación permite el análisis espectral de los registros adquiridos, obteniéndose un modelo representado por la curva de dispersión de cada emplazamiento, de modo que mediante una inversión se obtiene el modelo de velocidad de propagación en función de la profundidad. A través de estos modelos, pueden obtenerse otros parámetros de interés sismológico. Estos resultados se representan sobre mapas isométricos para obtener una relación espacial de los mismos, particularmente conocido como zonación sísmica. De este análisis se extrae que la VS30 promedio del Campus no es baja en exceso, correspondiéndose a posteriori con los resultados de amplificación sísmica, período fundamental de resonancia del lugar y profundidad del sustrato rocoso. En última instancia se comprueba que los valores de amplificación sísmica máxima y el período al cual se produce posiblemente coincidan con los períodos fundamentales de resonancia de algunos edificios del Campus. ABSTRACT In South Campus at Polytechnic University of Madrid, a project has been carried out to obtain a proper subsoil description by applying ReMi tests, in collaboration with the Department of Geophysics of the National Geographic Institute. Through geophysical tests conducted locally, the ReMi (Refraction Microtremor) technique allows to establish the physical parameters of soil, which are of special interest in the field of civil engineering. This technique is part of passive seismic methods, often used in geophysical prospecting. It focuses in obtaining the underlying model of propagation velocity distribution of the shear wave according to depth and has the advantage of being able to use seismic ambient noise as a source of energy. It was developed in the Nevada Seismological Laboratory (USA) by Louie (2001) as an innovative technique for obtaining propagation velocities experimentally. It has several other advantages, including the direct observation of the dispersion of surface waves, which allows to reliably measure S wave velocity. This is a non-invasive, low cost and good resolution method, which can be applied in urban or sensitive environments where other prospection methods present difficulties. The propagation velocity of shear waves in the first 30 meters Vs30 is widely recognized as a valid equivalent parameter to geotechnically characterize the subsurface. It is mathematically related to surface wave's velocity of propagation, which are to observe using REMI technique. Spectral analysis of acquired data sets up a model represented by the dispersion curve at each site, so that, using an inversion process, propagation velocity model in relation to depth is obtained. Through this models, other seismologically interesting parameters can be obtained. These results are represented on isometric maps in order to obtain a spatial relationship between them, a process which is known as seismic zonation. This analysis infers that Vs30 at South Campus is not alarmingly low , corresponding with subsequent results of seismic amplification, fundamental period of resonance of soil and depth of bedrock. Ultimately, it's found that calculated values of soil's fundamental periods at which maximum seismic amplification occurs, may possibly match fundamental periods of some Campus buildings.

Propuesta metodológica para el análisis y protección de la calidad del agua subterránea de acuerdo con los requerimientos de la Directiva Marco y la Directiva derivada de Aguas Subterráneas

La protección de las aguas subterráneas es una prioridad de la política medioambiental de la UE. Por ello ha establecido un marco de prevención y control de la contaminación, que incluye provisiones para evaluar el estado químico de las aguas y reducir la presencia de contaminantes en ellas. Las herramientas fundamentales para el desarrollo de dichas políticas son la Directiva Marco del Agua y la Directiva Hija de Aguas Subterráneas. Según ellas, las aguas se consideran en buen estado químico si: • la concentración medida o prevista de nitratos no supera los 50 mg/l y la de ingredientes activos de plaguicidas, de sus metabolitos y de los productos de reacción no supera el 0,1 μg/l (0,5 μg/l para el total de los plaguicidas medidos) • la concentración de determinadas sustancias de riesgo es inferior al valor umbral fijado por los Estados miembros; se trata, como mínimo, del amonio, arsénico, cadmio, cloruro, plomo, mercurio, sulfatos, tricloroetileno y tetracloroetileno • la concentración de cualquier otro contaminante se ajusta a la definición de buen estado químico enunciada en el anexo V de la Directiva marco sobre la política de aguas • en caso de superarse el valor correspondiente a una norma de calidad o a un valor umbral, una investigación confirma, entre otros puntos, la falta de riesgo significativo para el medio ambiente. Analizar el comportamiento estadístico de los datos procedentes de la red de seguimiento y control puede resultar considerablemente complejo, debido al sesgo positivo que suelen presentar dichos datos y a su distribución asimétrica, debido a la existencia de valores anómalos y diferentes tipos de suelos y mezclas de contaminantes. Además, la distribución de determinados componentes en el agua subterránea puede presentar concentraciones por debajo del límite de detección o no ser estacionaria debida a la existencia de tendencias lineales o estacionales. En el primer caso es necesario realizar estimaciones de esos valores desconocidos, mediante procedimientos que varían en función del porcentaje de valores por debajo del límite de detección y el número de límites de detección aplicables. En el segundo caso es necesario eliminar las tendencias de forma previa a la realización de contrastes de hipótesis sobre los residuos. Con esta tesis se ha pretendido establecer las bases estadísticas para el análisis riguroso de los datos de las redes de calidad con objeto de realizar la evaluación del estado químico de las masas de agua subterránea para la determinación de tendencias al aumento en la concentración de contaminantes y para la detección de empeoramientos significativos, tanto en los casos que se ha fijado un estándar de calidad por el organismo medioambiental competente como en aquéllos que no ha sido así. Para diseñar una metodología que permita contemplar la variedad de casos existentes, se han analizado los datos de la Red Oficial de Seguimiento y Control del Estado Químico de las Aguas Subterráneas del Ministerio de Agricultura, Alimentación y Medio Ambiente (Magrama). A continuación, y dado que los Planes Hidrológicos de Cuenca son la herramienta básica de las Directivas, se ha seleccionado la Cuenca del Júcar, dada su designación como cuenca piloto en la estrategia de implementación común (CIS) de la Comisión Europea. El objetivo principal de los grupos de trabajo creados para ello se dirigió a implementar la Directiva Derivada de Agua Subterráneas y los elementos de la Directiva Marco del Agua relacionadas, en especial la toma de datos en los puntos de control y la preparación del primer Plan de Gestión de Cuencas Hidrográficas. Dada la extensión de la zona y con objeto de analizar una masa de agua subterránea (definida como la unidad de gestión en las Directivas), se ha seleccionado una zona piloto (Plana de Vinaroz Peñiscola) en la que se han aplicado los procedimientos desarrollados con objeto de determinar el estado químico de dicha masa. Los datos examinados no contienen en general valores de concentración de contaminantes asociados a fuentes puntuales, por lo que para la realización del estudio se han seleccionado valores de concentración de los datos más comunes, es decir, nitratos y cloruros. La estrategia diseñada combina el análisis de tendencias con la elaboración de intervalos de confianza cuando existe un estándar de calidad e intervalos de predicción cuando no existe o se ha superado dicho estándar. De forma análoga se ha procedido en el caso de los valores por debajo del límite de detección, tomando los valores disponibles en la zona piloto de la Plana de Sagunto y simulando diferentes grados de censura con objeto de comparar los resultados obtenidos con los intervalos producidos de los datos reales y verificar de esta forma la eficacia del método. El resultado final es una metodología general que integra los casos existentes y permite definir el estado químico de una masa de agua subterránea, verificar la existencia de impactos significativos en la calidad del agua subterránea y evaluar la efectividad de los planes de medidas adoptados en el marco del Plan Hidrológico de Cuenca. ABSTRACT Groundwater protection is a priority of the EU environmental policy. As a result, it has established a framework for prevention and control of pollution, which includes provisions for assessing the chemical status of waters and reducing the presence of contaminants in it. The measures include: • criteria for assessing the chemical status of groundwater bodies • criteria for identifying significant upward trends and sustained concentrations of contaminants and define starting points for reversal of such trends • preventing and limiting indirect discharges of pollutants as a result of percolation through soil or subsoil. The basic tools for the development of such policies are the Water Framework Directive and Groundwater Daughter Directive. According to them, the groundwater bodies are considered in good status if: • measured or predicted concentration of nitrate does not exceed 50 mg / l and the active ingredients of pesticides, their metabolites and reaction products do not exceed 0.1 mg / l (0.5 mg / l for total of pesticides measured) • the concentration of certain hazardous substances is below the threshold set by the Member States concerned, at least, of ammonium, arsenic, cadmium, chloride, lead, mercury, sulphates, trichloroethylene and tetrachlorethylene • the concentration of other contaminants fits the definition of good chemical status set out in Annex V of the Framework Directive on water policy • If the value corresponding to a quality standard or a threshold value is exceeded, an investigation confirms, among other things, the lack of significant risk to the environment. Analyzing the statistical behaviour of the data from the monitoring networks may be considerably complex due to the positive bias which often presents such information and its asymmetrical distribution, due to the existence of outliers and different soil types and mixtures of pollutants. Furthermore, the distribution of certain components in groundwater may have concentrations below the detection limit or may not be stationary due to the existence of linear or seasonal trends. In the first case it is necessary to estimate these unknown values, through procedures that vary according to the percentage of values below the limit of detection and the number of applicable limits of detection. In the second case removing trends is needed before conducting hypothesis tests on residuals. This PhD thesis has intended to establish the statistical basis for the rigorous analysis of data quality networks in order to conduct the evaluation of the chemical status of groundwater bodies for determining upward and sustained trends in pollutant concentrations and for the detection of significant deterioration in cases in which an environmental standard has been set by the relevant environmental agency and those that have not. Aiming to design a comprehensive methodology to include the whole range of cases, data from the Groundwater Official Monitoring and Control Network of the Ministry of Agriculture, Food and Environment (Magrama) have been analysed. Then, since River Basin Management Plans are the basic tool of the Directives, the Júcar river Basin has been selected. The main reason is its designation as a pilot basin in the common implementation strategy (CIS) of the European Commission. The main objective of the ad hoc working groups is to implement the Daughter Ground Water Directive and elements of the Water Framework Directive related to groundwater, especially the data collection at control stations and the preparation of the first River Basin Management Plan. Given the size of the area and in order to analyze a groundwater body (defined as the management unit in the Directives), Plana de Vinaroz Peñíscola has been selected as pilot area. Procedures developed to determine the chemical status of that body have been then applied. The data examined do not generally contain pollutant concentration values associated with point sources, so for the study concentration values of the most common data, i.e., nitrates and chlorides have been selected. The designed strategy combines trend analysis with the development of confidence intervals when there is a standard of quality and prediction intervals when there is not or the standard has been exceeded. Similarly we have proceeded in the case of values below the detection limit, taking the available values in Plana de Sagunto pilot area and simulating different degrees of censoring in order to compare the results obtained with the intervals achieved from the actual data and verify in this way the effectiveness of the method. The end result is a general methodology that integrates existing cases to define the chemical status of a groundwater body, verify the existence of significant impacts on groundwater quality and evaluate the effectiveness of the action plans adopted in the framework of the River Basin Management Plan.

Novo procedimento para a realização de análise capwap no ensaio de carregamento dinâmico em estacas pré-moldadas.

Desde a década de 1980 diversos autores apresentaram correlações entre provas de carga estática e ensaios de carregamento dinâmico em estacas. Para uma boa correlação é fundamental que os testes sejam bem executados e que atinjam a ruptura segundo algum critério, como o de Davisson, por exemplo, além de levar em conta o intervalo de tempo entre a execução da prova de carga estática e do ensaio dinâmico, face ao efeito \"set up\". Após a realização do ensaio dinâmico realiza-se a análise CAPWAP que permite a determinação da distribuição do atrito lateral em profundidade, a carga de ponta e outros parâmetros dos solos tais como quakes e damping. A análise CAPWAP é realizada por tentativas através do procedimento \"signal matching\", isto é, o melhor ajuste entre os sinais de força medido pelos sensores e o calculado. É relativamente fácil mostrar que a mesma solução pode ser obtida através de dados de entrada diferentes. Isso significa que apesar de apresentarem cargas mobilizadas próximas o formato da curva da simulação de prova de carga estática, obtida pelo CAPWAP, assim como a distribuição do atrito lateral, podem ser diferentes, mesmo que as análises apresentem \"match quality\" (MQWU) satisfatórios. Uma forma de corrigir o formato da curva simulada do CAPWAP, assim como a distribuição do atrito lateral, é através da comparação com provas de carga estática (PCE). A sobreposição das duas curvas, a simulada e a \"real\", permite a determinação do quake do fuste através do trecho inicial da curva carga-recalque da prova de carga estática, que por sua vez permite uma melhor definição da distribuição do atrito lateral e da reação de ponta. Neste contexto surge o conceito de \"match quality de recalques\" (MQR). Quando a PCE não está disponível, propõe-se efetuar um carregamento estático utilizando o peso próprio do martelo do bate-estaca (CEPM). Mostra-se, através de dois casos de obra, em que estavam disponíveis ensaios de carregamento dinâmico e PCEs, que esse procedimento permite obter uma melhor solução do ponto de vista físico, isto é consistente com as características do subsolo e com a curva carga-recalque da PCE, e não apenas matemático, através da avaliação do \"match quality\" (MQWU).

Relationship between piezometric level and ground deformations measured by means of DInSAR in the Vega Media of the Segura River (Spain)

Differential SAR Interferometry (DInSAR) is a remote sensing method with the well demonstrated ability to monitor geological hazards like earthquakes, landslides and subsidence. Among all these hazards, subsidence involves the settlement of the ground surface affecting wide areas. Frequently, subsidence is induced by overexploitation of aquifers and constitutes a common problem that affects developed societies. The excessive pumping of underground water decreases the piezometric level in the subsoil and, as a consequence, increases the effective stresses with depth causing a consolidation of the soil column. This consolidation originates a settlement of ground surface that must be withstood by civil structures built on these areas. In this paper we make use of an advanced DInSAR approach - the Coherent Pixels Technique (CPT) [1] - to monitor subsidence induced by aquifer overexploitation in the Vega Media of the Segura River (SE Spain) from 1993 to the present. 28 ERS-1/2 scenes covering a time interval of about 10 years were used to study this phenomenon. The deformation map retrieved with CPT technique shows settlements of up to 80 mm at some points of the studied zone. These values agree with data obtained by means of borehole extensometers, but not with the distribution of damaged buildings, well points and basements, because the occurrence of damages also depends on the structural quality of the buildings and their foundations. The most interesting relationship observed is the one existing between piezometric changes, settlement evolution and local geology. Three main patterns of ground surface and piezometric level behaviour have been distinguished for the study zone during this period: 1) areas where deformation occurs while ground conditions remain altered (recent deformable sediments), 2) areas with no deformation (old and non-deformable materials), and 3) areas where ground deformation mimics piezometric level changes (expansive soils). The temporal relationship between deformation patterns and soil characteristics has been analysed in this work, showing a delay between them. Moreover, this technique has allowed the measurement of ground subsidence for a period (1993-1995) where no instrument information was available.

Effect of water vapour condensation on the radon content in subsurface air in a hypogeal inactive-volcanic environment in Galdar cave, Spain

Fluctuations of trace gas activity as a response to variations in weather and microclimate conditions were monitored over a year in a shallow volcanic cave (Painted Cave, Galdar, Canary Islands, Spain). 222Rn concentration was used due to its greater sensitivity to hygrothermal variations than CO2 concentration. Radon concentration in the cave increases as effective vapour condensation within the porous system of the rock surfaces inside the cave increases due to humidity levels of more than 70%. Condensed water content in pores was assessed and linked to a reduction in the direct passage of trace gases. Fluctuations in radon activity as a response to variations in weather and microclimate conditions were statistically identified by clustering entropy changes on the radon signal and parameterised to predict radon concentration anomalies. This raises important implications for other research fields, including the surveillance of shallow volcanic and seismic activity, preventive conservation of cultural heritage in indoor spaces, indoor air quality control and studies to improve understanding of the role of subterranean terrestrial ecosystems as reservoirs and/or temporary sources of trace gases.

Using quantity/intensity relationships to assess the potential for ammonium leaching in a Vertosol

High concentrations of ammonium (up to 0.1 cmol/kg) have been observed below 1 m depth in a Vertosol soil near Warra in south-eastern Queensland. This study examined whether ammonium leaching could be responsible for the ammonium accumulation observed in the Warra soil. This was done by using quantity/intensity (Q/I) relationships to compare the ammonium retention capacity of the Warra soil with other similar soils throughout the region that did not contain elevated subsoil ammonium concentrations. Analysis of Q/I curves revealed that in the concentration range studied, the amount of ammonium retained on high affinity adsorption sites in all 3 soils was low, and the Warra soil was not significantly different from the other 2 soils. The ability of the soils to retain ammonium in the soil solution against leaching [i.e. their potential buffer capacity (PBC)] did differ between soils and was greatest at Warra. This indicates that at any one time the Warra soil holds more ammonium on the exchange complex and less in solution than the other soils examined. It was concluded that ammonium is no more likely to leach through the surface horizons of the Warra soil than the other soils examined. Indeed, the data indicated that the Warra soil probably has greater capacity to retain ammonium against leaching due to its greater PBC. Consequently, it is considered unlikely that leaching of ammonium has been a major contributor to the subsoil ammonium concentrations at Warra.

Dissipation of acetochlor and its distribution in surface and sub-surface soil fractions during laboratory incubations

Pesticides in soil are subject to a number of processes that result in transformation and biodegradation, sorption to and desorption from soil components, and diffusion and leaching. Pesticides leaching through a soil profile will be exposed to changing environmental conditions as different horizons with distinct physical, chemical and biological properties are encountered. The many ways in which soil properties influence pesticide retention and degradation need to be addressed to allow accurate predictions of environmental fate and the potential for groundwater pollution. Degradation and sorption processes were investigated in a long-term (100 days) study of the chloroacetanilide herbicide, acetochlor. Soil cores were collected from a clay soil profile and samples taken from 0-30cm (surface), 1.0-1.3m (mid) and 2.7-3.0m (deep) and treated with acetochlor (2.5, 1.25, 0.67 mu g acetochlor g(-1) dry wt soil, respectively). In sterile and non-sterile conditions, acetochlor concentration in the aqueous phase declined rapidly from the surface and subsoil layers, predominantly through nonextractable residue (NER) formation on soil surfaces, but also through biodegradation and biotic transformation. Abiotic transformation was also evident in the sterile soils. Several metabolites were produced, including acetochlor-ethane sulphonic acid and acetochlor-oxanilic acid. Transformation was principally microbial in origin, as shown by the differences between non-sterile and sterile soils. NER formation increased rapidly over the first 21 days in all soils and was mainly associated with the macroaggregate (> 2000 mu m diameter) size fractions. It is likely that acetochlor is incorporated into the macroaggregates through oxidative coupling, as humification of particulate organic matter progresses. The dissipation (ie total loss of acetochlor) half-life values were 9.3 (surface), 12.3 (mid) and 12.6 days (deep) in the non-sterile soils, compared with 20.9 [surface], 23.5 [mid], and 24 days [deep] in the sterile soils, demonstrating the importance of microbially driven processes in the rapid dissipation of acetochlor in soil.

Hydraulic properties of layered soils influence survival of Rhodes grass (Chloris gayana Kunth.) during water stress

Survival of vegetation on soil-capped mining wastes is often impaired during dry seasons due to the limited amount of water stored in the shallow soil capping. Growth and survival of Rhodes grass (Chloris gayana) during soil drying on various layered capping sequences constructed of combinations of topsoil, subsoil, seawater-neutralised residue sand and low grade bauxite was determined in a glasshouse. The aim was to describe the survival of Rhodes grass in terms of plant and soil water relationships. The soil water characteristic curve and soil texture analysis was a good predictor of plant survival. The combination of soil with a high water holding capacity and low soil water diffusivity (e.g. subsoil with high clay contents) with soil having a high water holding capacity and high diffusivity (e.g. residue sand) gave best survival during drying down (up to 88 days without water), whereas topsoil and low grade bauxite were unsuitable (plants died within 18-39 days). Clayey soil improved plant survival by triggering a water stress response during peak evaporative water demand once residue sand dried down and its diffusivity fell below a critical range. Thus, for revegetation in seasonally dry climates, soil capping should combine one soil with low diffusivity and one or more soils with high total water holding capacity and high diffusivity.

Rice growth and post-rice mungbean in relation to two puddling intensities under glasshouse conditions

The effect of soil puddling on growth of lowland rice (Oryza sativa) and post-rice mungbean (Vigna radiata) was investigated using mini rice beds under controlled glasshouse conditions. Each mini rice bed was approximately 1 m(3) in size. Three different soil types were used: a well-drained, permeable loam; a hardsetting, structurally unstable silty loam; and a medium clay. Rice yields were reduced by low puddling compared with high puddling intensity on the loam but not affected on the heavier textured soils (silty loam and clay). Yield of mungbean was reduced on highly puddle, structurally unstable soil, indicating that puddling should be reduced on structurally unstable soils. Under glasshouse condition where crop establishment was not a limiting factor and plant available water in 0.65 m of soil was 100 mm, mungbean yields of >1 t/ha were achieved. However, under conditions where subsoil water reserves were depleted for the production of vegetative biomass during initial optimal growing condition, grain yield remained well below 1 t/ha.

Avaliação da compactação do solo no crescimento inicial de espécies florestais da caatinga

Despite the importance of the study of roots, little is known about the negative effects of soil compaction in the development of the Caatinga forest species. In this sense, the objective was to evaluate the initial growth of Mimosa caesalpiniifolia, Tabebuia caraiba and Erythina velutina in soil under varying levels of compression. The experiment was conducted in a greenhouse located at the Academic Unit Specialized in Agricultural Sciences, UFRN. To perform the experiment, was used Oxisoil of sandy loam texture, from forest trial Area Agricultural School of Jundiaí (EAJ) of the municipality of Macaíba-RN, in an experimental unit consisting of three overlapping PVC rings, 10 cm in diameter and 25 cm in height, with a central ring which has undergone compression. The experimental design was a randomized block with six replications, being tested four levels of soil compaction (1.35; 1.45; 1.60 and 1.80 kg.dm-³), evaluating the following variables: diameter, height, number of leaves, dry weight of shoot and root system in each layer of the vessels. Overall, the species M. caesalpiniifolia, T. caraiba and E. velutina had initial growth favored by treatment consists of uncompressed soil. The M. caesalpiniifolia and T. caraiba species proved relatively resistant to compaction of the soil does not undergo any significant reduction in root growth density equal to or less than 1.60 kg.dm-³, whereas E. velutina proved susceptible effects of soil compaction, with significant changes in root growth under soil densities equal to or greater than 1.45 kg.dm-³. Increased soil compaction caused the impediment to the expansion of taproot inside the experimental units, promoting the accumulation of roots in the upper layers of the soil for the studied species. The subsoil physical impediment changed the initial aerial growth of M. caesalpiniifolia and E. velutina, but did not influence the growth of air T. caraiba seedlings the tested compression levels.