「住民参加」によるアフリカ熱帯雨林の保全と開発に向けて -- ガボン南西部ムカラバ・ドゥドゥ国立公園の事例から

アフリカ熱帯雨林とそこにすむ野生動物の保全は喫緊の国際課題であるが、政情不安や経済の停滞にくわえ、地域住民との軋轢が保全政策の大きな障害となっている。有効な保全体制を構築するためには、地域の社会的文脈をふまえ、地域コミュニティごとに固有の特徴と地域住民の多様性を理解することが重要である。そこで筆者は、ガボンの国立公園を対象に、地域コミュニティの歴史的・文化的背景および住民生活の実態について調べた。その結果、(1)地域コミュニティは、その歴史的・文化的背景により、出自や経歴が多様な人々から構成される流動的なものであること、(2)住民生活は、伝統的な自然資源利用を基盤としながらも、伐採事業や保全事業に強く影響を受けていることが明らかになった。一枚岩的な地域住民を前提とした「住民参加」概念を外部から当てはめるのではなく、地域社会の実態に即して内部からコミュニティを抽出し、それをもとに保全と開発事業を進める必要があるといえる。

The Extended Water Footprint and illegal groundwater use in the Upper Guadiana Basin (Spain)

Tablas de Daimiel National Park is located in the Upper Guadiana Basin and represents one of the largest and most important wetlands in Europe. The long term ecological integrity of this wetland is inherently associated with the maintenance of a shallow groundwater table, namely the Western Mancha aquifer (WMA) or Aquifer 23. The intensive use of groundwater, mainly for irrigation, has led over the last decades to deep socio‐economic changes. Such intensive use has also lowered the water table of Aquifer 23, drastically reducing the flooded area of the wetland and threatening its ecological integrity. A number of plans and measures have been developed and implemented since the declaration of overexploitation of Aquifer 23 in the year 1987. The most recent one is the Special Plan for the Upper Guadiana (SPUG), approved in 2008. This Plan is the main measure to comply with achieving the objective of good quantitative and qualitative status required under the Water Framework Directive (2000). This paper offers a new type of integrated analysis which allows assessing under a common lens the physical, economic and social dimensions of groundwater use in the area. The first objective is to calculate the groundwater footprint of agricultural production in the Upper Guadiana basin and its evolution during 2000‐2008. For this purpose, we have applied the Extended Water Footprint (EWF) methodology ‐a novel approach based on the classical Water Footprint (WF) approach‐ that includes an assessment of the water productivity from an economic and social perspective. Compared to the classical WF, the EWF allows for a more complete overview of the sector, providing new insights for policy decisions (e.g. to define options and possibilities on water re‐allocation in order to achieve both better ecosystem conservation and social equity). The second objective is to use the EWF to compare the existing authorized and non‐authorized or illegal use of water. This allows us to discuss current initiatives by public authorities in relation to the existing frame of water rights

Investigaciones dendrogeomorfológicas aplicadas al estudio de la peligrosidad por avenidas e inundaciones en el parque nacional de la Caldera de Taburiente (La Palma, Islas Canarias).

Las Angustias torrent is an ungauged stream located in the Caldera de Taburiente National Park (Canary Islands), where frequent and intense flood events occur (even causing fatalities, such as in November 2001). The aim of this research is to analyse the flood hazard in one of the most visited areas of this protected area. To carry out this objective, during two dendrogeomorphological campaigns, all pine trees located on the stream bed and banks showing external evidence of flash flood damage were sampled. In addition, a detailed topographical survey using GPS and total station allowed us to obtain the inputs for hydraulic modelling. In the preliminary results, two flood events have been identified (1967-1968 and 1999- 2000), and evidence of other dates has been observed (1976, 1983, 1993 and 2001). Magnitude reconstruction of these events will improve flood hazard and risk analyses and will be useful for National Park managers.

Geomorphological analysis and evolution of an altered floodplain drainage system. The case of the Partido Stream (Spain)

The Partido Stream is a small torrential course that flows into the marsh of the Doñana National Park, an area that was declared a World Heritage Site in 1994. Before 1981, floods occurred, and the stream overflowed onto a floodplain. As an old alluvial fan, the floodplain has its singular orography and functionality. Fromthe floodplain, several drainage channels, locally called caño, discharged into themarsh. The Partido Streamhad themorphology of a caño and covered approximately 8 km from the old fan to the marsh. The stream was straightened and channelised in 1981 to cultivate the old fan. This resulted in floods that were concentrated between the banks in the following years, which caused the depth of water and the shear stress to increase, thus, scouring the river bed and river banks. In this case, the eroded materials were carried towards the marsh where a new alluvial fan evolved. Control measures on the old fan were implemented in 2006 to stop the development of the new alluvial fan downstream over the marsh. Thus, the stream would partially recover its original behaviour that it had before channelisation, moving forwards in a new, balanced state. The present study describes the geomorphological evolution that channelisation has caused since 1981 and the later slow process of recovery of the original hydraulic-sedimentation regime since 2006. Additionally, it deepens the understanding of the original hydraulic behaviour of the stream, combining field data and 2D simulations.

Evaluación del ruido ambiental en espacios naturales protegidos: implicaciones para su gestión

Esta Tesis Doctoral trata sobre la caracterización acústica de los ecosistemas naturales y la evaluación del impacto ambiental del ruido antropogénico sobre sus potenciales receptores en estos lugares, incluidos los receptores no humanos y sus efectos ecológicos, además, analiza las implicaciones para su gestión a distintas escalas y se lleva a cabo una valoración económica. Este trabajo ofrece soluciones para caracterizar los paisajes sonoros de forma compatible con distintas escalas de trabajo, nivel de esfuerzo técnico y en contextos de recursos limitados que haga viable su tratamiento como cualquier otra variable ambiental en el ámbito de la conservación y gestión del medio natural. Se han adaptado herramientas y metodologías propias de disciplinas como la acústica ambiental, bioacústica y ecología del paisaje, para servir a los objetivos específicos de la evaluación y gestión de los paisajes sonoros y el ruido ambiental en amplias extensiones geográficas. Se ha establecido un método general de muestreo sistemático para trabajo de campo y también se han adaptado métodos de modelización informática, que permiten analizar escenarios sonoros dinámicos en el tiempo y en el espacio, desde localizaciones puntuales hasta la escala del paisaje. Es posible elaborar cartografía ambiental con esta información y se ha representado gráficamente la zona de influencia de distintas fuentes de ruido sobre la calidad de distintos hábitats faunísticos. Se recomienda el uso del indicador del nivel de presión sonora equivalente (Leq) por su operatividad en medición y modelización, y su adaptabilidad a cualquier dimensión espacial y temporal que se requiera, por ejemplo en función del paisaje, actividades o especies que se establezcan como objeto de análisis. Se ha comprobado que las voces y conversaciones de parte de los excursionistas en zonas de reposo, observación y descanso (Laguna Grande de Peñalara) es la fuente de ruido que con mayor frecuencia identifican los propios visitantes (51%) y causa un incremento del nivel de presión sonora equivalente de unos 4,5 dBA sobre el nivel correspondiente al ambiente natural (Lnat). También se ha comprobado que carreteras con bajo nivel de tráfico (IMD<1000) pueden causar estrés fisiológico sobre la fauna y afectar a la calidad de sus hábitats. La isófona de 30 dBA del índice Leq (24h) permite dividir a los corzos de la zona de estudio en dos grupos con diferente nivel de estrés fisiológico, más elevado en los que se sitúan más cerca de la carretera con mayor volumen de tráfico y se expone a mayores niveles de ruido. Por otro lado, ha sido posible delimitar una zona de exclusión para la nidificación de buitre negro alrededor de las carreteras, coincidente con la isófona Leq (24h) de 40 dBA que afecta al 11% de su hábitat potencial. Además se ha llevado a cabo una novedosa valoración económica de la contaminación acústica en espacios naturales protegidos, mediante el análisis de la experiencia sonora de los visitantes del antiguo Parque Natural de Peñalara, y se ha constatado su disposición al pago de una entrada de acceso a estos lugares (aproximadamente 1 euro) si redundara en una mejora de su estado de conservación. En conclusión, los espacios naturales protegidos pueden sufrir un impacto ambiental significativo causado por fuentes de ruido localizadas en su interior pero también lejanas a ellos, que se sitúan fuera del ámbito de competencias de sus gestores. Sucesos sonoros como el sobrevuelo de aviones pueden incrementar en aproximadamente 8 dBA el nivel de referencia Lnat en las zonas tranquilas del parque. Se recomienda llevar a cabo una gestión activa del medio ambiente sonoro y se considera necesario extender la investigación sobre los efectos ecológicos del ruido ambiental a otros lugares y especies animales. ABSTRACT This PhD Thesis deals with acoustic characterization of natural ecosystems and anthropogenic noise impact assessment on potential receivers, including non-human receivers and their ecological effects. Besides, its management implications at different scales are analyzed and an economic valuation is performed. This study provides solutions for characterizing soundscapes in a compatible way with different working scales, level of technical effort and in a context of limited resources, so its treatment becomes feasible as for any other environmental variable in conservation and environmental management. Several tools and methodologies have been adapted from a variety of disciplines such as environmental acoustics, bioacoustics and landscape ecology, to better serve the specific goals of assessing and managing soundscapes and environmental noise in large areas. A procedure has been established for systematic field measurement surveys and noise common computer modelling methods have also been adapted in order to analyze dynamic soundscapes across time and space, from local to landscape scales. It is possible to create specific thematic cartography as for instance delimiting potential influence zone from different noise sources on animal habitats quality. Use of equivalent continuous sound pressure level index (Leq) is recommended because it provides great flexibility in operation for noise measurement and modelling, and because of its adaptability to any required temporal and spatial dimension, for instance landscape, activities or the target species established as study subjects. It has been found that human voices and conversations in a resting and contemplation area (Laguna Grande de Peñalara) is the most frequently referred noise source by national park visitors (51 %) when asked. Human voices alter this recreational area by increasing the sound pressure level approximately 4.5 dBA over the natural ambient level (Lnat). It has also been found that low traffic roads (AADT<1000 ) may cause physiological stress on wildlife and affect the quality of their habitats. It has also been possible to define a road-effect zone by noise mapping, which suggests an effective habitat loss within the Leq (24h) 30 dBA isophone in case of Roe deer and also divide the study area in two groups with different physiological stress level, higher for those exposed to higher noise levels and traffic volume. On the other hand, it has been possible to determine an exclusion area for Cinereous vulture nesting surrounding roads which is coincident with the Leq (24h) 40 dBA isophone and affects 11 % of the vulture potential habitat. It has also been performed an economic estimation of noise pollution impact on visitors’ perception and results showed that visitors would be willing to pay an entrance fee of approximately 1 euro if such payment is really bringing an improvement of the conservation status. In conclusion, protected areas may be significantly affected by anthropogenic noise sources located within the park borders but perturbations may also be caused by large-distance noise sources outside the park managers’ jurisdiction. Aircraft overflight events disrupted quietness and caused Leq increases of almost 8 dBA during a monitoring period with respect to Lnat reference levels in the park quiet areas. It is recommended to actively manage the acoustic environment. Finally, further research on ecological impacts of environmental noise needs to be extended to other species and places.

Alteración del comportamiento hidráulico natural de la vertiente noreste de la marisma de El Rocío por efectos antrópicos

El geo-dinamismo torrencial es resultado de la incidencia de precipitaciones torrenciales en la cuenca hidrográfica, y se manifiesta por una intensificación del ciclo del agua (con la presencia de mayores volúmenes de escorrentía y la consiguiente aparición de repentinos y elevados caudales de avenida) e intensificación del ciclo de los sedimentos (mayor erosión del suelo, incremento del transporte de sedimentos en los cauces de drenaje y la formación de grades depósitos de sedimentos en el área dominada de la cuenca). Estos procesos naturales se pueden agravar si se realizan en la cuenca actuaciones que alteren sustancialmente su morfología; es el caso del arroyo del Partido, tributario a la marisma de El Rocío en el Parque Nacional de Doñana, cuyo encauzamiento del tramo final sobre su antiguo cono de sedimentación fue el causante de la formación de un nuevo cono de sedimentación sobre la marisma. Pero las intervenciones antrópicas también pueden dirigir el sistema hacia la estabilidad sedimentaria y el tramo final del arroyo del Partido ha experimentado asimismo actuaciones de carácter restaurador. El antiguo cono de sedimentación del arroyo del Partido es un lugar complejo en el que drenan también otros tres cursos que intercambian sus flujos con dicho arroyo durante las avenidas. Esta Memoria analiza cuatro situaciones del paraje objeto de estudio: la primera responde al estado original del lugar en cuestión (situación A); la segunda a la creada tras el encauzamiento del arroyo del Partido en 1981 (situación B); la tercera a la formada pasado un tiempo desde el encauzamiento, cuando el geo-dinamismo del lugar hizo sus efectos sobre el paraje en cuestión (situación C); y la cuarta la generada tras la restauración en el verano de 2006 del régimen hidráulico-sedimentario del arroyo del Partido con la Actuación núm. 3 del Proyecto Doñana 2005. Se han investigado los efectos que la alteración de la morfología del sistema de drenaje del antiguo cono de sedimentación del arroyo del Partido causa en los parámetros hidráulicos que desencadenan el geo-dinamismo torrencial. Para ello se han reproducido las condiciones morfológicas de las cuatro situaciones más representativas ya comentadas que ha experimentado el paraje en los últimos 30 años y que han condicionado el comportamiento de las avenidas torrenciales ocurridas en dicho periodo. En este contexto se ha elaborado un modelo hidrológico con el programa HECHMS a partir de la información disponible y un modelo hidrodinámico en 2D con el programa IBER; con este último se han comparado ocho escenarios característicos derivados de la incidencia de dos avenidas representativas de los eventos torrenciales de la zona sobre las morfologías contempladas. También se ha estudiado la tensión de arrastre de las avenidas dada su incidencia en el terreno sobre el que transitan, analizando de manera separada los efectos en los cuatro cauces de drenaje del antiguo cono de sedimentación y del resto de la superficie del mismo. La investigación realizada ha permitido describir minuciosamente el comportamiento de los drenajes locales del antiguo y complejo cono de sedimentación que bordea el noroeste de la marisma del Parque Nacional de Doñana, desde la marisma de El Rocío hasta la marisma gallega, lo que redundará en beneficio de la gestión del Parque Nacional de Doñana y de su entorno, y especialmente en la seguridad del perímetro oriental de la aldea de El Rocío. ABSTRACT The torrential geo-dynamism results from the effect of torrential precipitations on the hydrological watershed, and it shows ups with the intensification of the water cycle (with presence of higher volumes of run-off and the consequent appearance of sudden and high food flows) and intensification of the sediment cycle (higher soil erosion, increase of sediment transport in the drainage courses and the formation of big sediment deposits in the area downstream the watershed). These natural processes can worsen if actions that change the morphology of the watershed are carried out. It is the case of the Partido stream, tributary of the marsh of El Rocío in the Doñana National Park, whose channelization of the final stretch over its old alluvial fan was the cause of the formation of a new alluvial fan over the marsh. But human actions can also go toward the sediment stabilization, and the final stretch of the Partido stream has experienced restoration actions as well. The old alluvial fan of the Partido stream is a complex terrain where also other three courses exchange their flows during floods. This document analyses four situations of the area studied: the first corresponds to the original state of the place (situation A); the second is the state created after the channel of the Partido stream was built in 1981 (situation B); the third is the state formed after some time passed and the geo-dynamism caused effect in the channelization (situation C); and the forth situation is the one created after the restoration in summer of 2006 of the hydraulic-sedimentary regime of the Partido stream with de Action number 3 of the Doñana 2005 Project. It has been researched the effects that the alteration of the morphology of the drainage system of the old alluvial fan of the Partido stream causes to the hydraulic parameters that trigger the torrential geo-dynamism. For that, the morphologic conditions of the four more representative situations were reproduced. Those situations experienced in the area in the last 30 years have conditioned the behaviour of torrential floods in that period. In this context, a hydrologic model with HEC-HMS and a 2D hydro-dynamic model with IBER have been set up. With IBER, eight scenes have been compared resulting from the impact of two representative floods from torrential events in the region against the morphologies considered. Also, the shear stress of the floods on the terrain has been studied, analysing separately the effect in the four drainage courses of the old alluvial fan and in the rest of its surfaces. The research carried out has allowed describing in minute detail the behavior of the local drainages of the old and complex alluvial fan that border the northwest part of the marsh of Doñana National Park, from the marsh of El Rocío to the gallega marsh. This will result in benefit for the management of Doñana National Park and its surroundings, and especially for the safety of the eastern limit of El Rocío village.

Unravelling past flash flood activity in a forested mountain catchment of the Spanish Central System

Flash floods represent one of the most common natural hazards in mountain catchments, and are frequent in Mediterranean environments. As a result of the widespread lack of reliable data on past events, the understanding of their spatio-temporal occurrence and their climatic triggers remains rather limited. Here, we present a dendrogeomorphic reconstruction of past flash flood activity in the Arroyo de los Puentes stream (Sierra de Guadarrama, Spanish Central System). We analyze a total of 287 increment cores from 178 disturbed Scots pine trees (Pinus sylvestris L.) which yielded indications on 212 growth disturbances related to past flash flood impact. In combination with local archives, meteorological data, annual forest management records and highly-resolved terrestrial data (i.e., LiDAR data and aerial imagery), the dendrogeomorphic time series allowed dating 25 flash floods over the last three centuries, with a major event leaving an intense geomorphic footprint throughout the catchment in 1936. The analysis of meteorological records suggests that the rainfall thresholds of flash floods vary with the seasonality of events. Dated flash floods in the 20th century were primarily related with synoptic troughs owing to the arrival of air masses from north and west on the Iberian Peninsula during negative indices of the North Atlantic Oscillation. The results of this study contribute considerably to a better understanding of hazards related with hydrogeomorphic processes in central Spain in general and in the Sierra de Guadarrama National Park in particular.