Research Note:<br>An approach to integrated assessement of reservoir siltation: the Joaquín Costa reservoir as a case study

International audienceIn 1932, the Esera river was dammed at the foothills of the Pyrenean External Ranges; since then, sedimentation has reduced its water storage capacity by a third. This study of the sediments in the Joaquín Costa reservoir has been based on detailed sedimentological examination and other analysis of mineralogy, grain size distribution and the chemical components of the materials accumulated at the bottom of the reservoir. Interpretations are based on results from four sediment cores collected at sites representative of the main environments in the reservoir. Records of known flood events and of reservoir management data have been combined with a 137Cs-derived chronology. Thus, it has been possible to ascribe the sedimentary record at the different reservoir environments to specific years, as well as some main changes in the facies types and sediment components. This methodology is a first approach to assessing siltation processes and dynamics in Mediterranean mountain reservoirs. Keywords: reservoir siltation, mineralogy, sedimentology,sedimentation rates, 137Cs, sediment tracing, mountain reservoir, central Spanish Pyrenee

Análisis sedimentológico del embalse de Barasona, Huesca

[Resumen] La pérdida de capacidad debido al aterramiento es un grave problema en numerosos embalses. El pantano de Barasona, en la cuenca del Esera-Isábena, Pirineos Centrales, uno de los más antiguos de España, ha perdido un tercio de su 3 capacidad inicial (71 Hm ) desde su construcción en 1932. El estudio de 23 sondeos ha permitido caracterizar el sedimento,definir facies sedimentarias, reconstruir tridimensionalmente el relleno del vaso y proponer un modelo deposicional dominado por las fluctuaciones en el régimen de aporte de los ríos. Las variaciones en la composición mineralógica proporcionan información sobre áreas fuente y procesos de erosión y transporte en la cuenca. Correlacionando los niveles de limos arenosos con los episodios de avenidas, se ha construido una cronología preliminar que permitirá evaluar variaciones en la tasa de aporte de sedimentos al embalse y en la dinámica del sistema embalse-cuenca..[Abstract] Sediment deliver and consequent loss of water storage capacity aggravate reservoir management problems. The Barasona reservoir in the Esera-Isabena watershed, Central Pyrenees, is one of the oldest in Spain (1932) and has lost one 3 third of its initial water capacity (71 Hm ). In this study we analyze the composition of the infilling of the Barasona reservoir, identify sedimentary facies, and reconstruct the tri-dimensional geometry based on 23 cores. Sedimentary dynamics is mainly controlled by fluctuations in the river inflow. Changes in mineral composition inform of sediment provenance and transport processes in the catchment area. A preliminary chronology based on the identification of floods in the sedimentary record (sandy silt layers) will allow to investigate changes in the sediment yield and in the interaccions reservoir-catchment

Influence of hail suppression systems over silver content in the environment in Aragón (Spain). II: Water, sediments and biota

The silver content in soils in the area in the surroundings of the Gallocanta Lake (Aragón, NE Spain) is lower than expected considering the estimated silver emission during the last 50 years by hail suppression systems. To understand the silver accumulation processes, selected water (4 surface, 3 groundwater), biota and sediment (6 surface sediments and 3 cores from Gallocanta and Campillo de Dueñas Lakes and Used Reservoir) samples have been analysed. An essay comparing the growth of wheat in pots with different silver iodide concentrations has been carried out. Finally, silver content in 7 tissues from two sheep that graze in areas both with and without hail suppression systems during 6–8 years were analysed. Our results show that after 50 years of silver iodide emissions to the atmosphere, silver accumulation in the waters and sediments of the lowlands, including some wetlands of high ecological value, has not been significant. Sediment cores did not show any peaks associated to silver emission. We propose that constant absorption of silver by plants could explain the low concentration in water and sediments. Crops and grass could accumulate the excess silver, as both wheat and sheep are able to absorb significant amounts of silver. These bio - accumulation processes could have helped to avoid a progressive environmental deterioration of the surroundings of the Gallocanta Lake. However, this hypothesis should be corroborated and quantified by further research on the analysis of natural and agricultural areas under the influence of hail suppression systems

Limnogeologúa de Laguna Chungará y cambio climático durante el Holoceno superior en el altiplano chileno septentrional

[Resumen] El estudio sísmico de la Laguna Chungará (69° 30' O, 18° 15'S, 4520 m. s.n.m, Altiplano chileno septentrional) y el análisis sedimentológico de varios sondeos ha permitido reconstruir la evolución de la sedimentación lacustre en el lago durante el Holoceno Superior. Se han identificado dos asociaciones de facies: i) litoral, más somera, compuesta por facies de turbera y in plataforma lacustre, más profunda, compuesta por facies con abundantes fragmentos de Characeae. Estas facies alternan en tres ciclos sedimentarios provocados por fluctuaciones en el nivel del lago. Estas variaciones hidrológicas en la laguna han sido causadas por cambios en el balance hídrico que a su vez reflejan importantes fluctuaciones climáticas durante el Holoceno Superior.[Abstract] We reconstruct the Late Holocene sedimentary history of Laguna Chungará (69° 30' W, 18° 10'5, 4520 m.a.s.l., northern Chilean Altiplano) based on high resolution seismic profiling and sedimentologic analyses of cores. Two sedimentary facies associations have been defined and interpreted: n macrophytedominant littoral, composed of black muds with macrophyte remains and peaty muds, and in Characeae-dominant lacustrine self, composed of gray muds and sands with abundant Characeae remains. The two facies associations define three cycles caused by oscillations in the lake level from shallower (macrophyte) to deeper (Characeae) conditions. Changes in the hydrology of Laguna Chungará reflect variations in the effective moisture (precipitation - evaporation) in the Altiplano during the Late Holocene

Hacia una enseñanza universitaria participativa y no jerarquizada : desarrollo de un método activo-solidario. Un ejemplo en la enseñanza de la Petrología

Presentamos una experiencia didáctica realizada en la Universidad de Zaragoza con el alumnado de tercero de Ciencias Geológicas, en un curso cuatrimestral de Petralogía de Rocas Sedimentarias y Metamórficas. Pretendemos demostrar que es posible una enseñanza de calidad en la que una mayoría de los estudiantes desarrollen el máximo de sus potencialidades.We want to presente a didactic experiment wich was carried put for a term in a course on "Exogenous and Metamorphic Rock petrology" within the third tear of Geological Studies. Our experiment tries to show the likeliness of a kind of university studies where students can have a greater share and therefore develop their full potentiality

Hacia una enseñanza universitaria participativa y no jerarquizada : desarrollo de un método activo-solidario. Un ejemplo en la enseñanza de la Petrología

Presentamos una experiencia didáctica realizada en la Universidad de Zaragoza con el alumnado de tercero de Ciencias Geológicas, en un curso cuatrimestral de Petralogía de Rocas Sedimentarias y Metamórficas. Pretendemos demostrar que es posible una enseñanza de calidad en la que una mayoría de los estudiantes desarrollen el máximo de sus potencialidades.We want to presente a didactic experiment wich was carried put for a term in a course on "Exogenous and Metamorphic Rock petrology" within the third tear of Geological Studies. Our experiment tries to show the likeliness of a kind of university studies where students can have a greater share and therefore develop their full potentiality

Late Holocene climate variability in the southwestern Mediterranean region: an integrated marine and terrestrial geochemical approach

A combination of marine (Alboran Sea cores, ODP 976 and TTR 300 G) and terrestrial (Zoñar Lake, Andalucia, Spain) geochemical proxies provides a high-resolution reconstruction of climate variability and human influence in the southwestern Mediterranean region for the last 4000 years at inter-centennial resolution. Proxies respond to changes in precipitation rather than temperature alone. Our combined terrestrial and marine archive documents a succession of dry and wet periods coherent with the North Atlantic climate signal. A dry period occurred prior to 2.7 cal ka BP – synchronously to the global aridity crisis of the third-millennium BC – and during the Medieval Climate Anomaly (1.4–0.7 cal ka BP). Wetter conditions prevailed from 2.7 to 1.4 cal ka BP. Hydrological signatures during the Little Ice Age are highly variable but consistent with more humidity than the Medieval Climate Anomaly. Additionally, Pb anomalies in sediments at the end of the Bronze Age suggest anthropogenic pollution earlier than the Roman Empire development in the Iberian Peninsula. The Late Holocene climate evolution of the in the study area confirms the see-saw pattern between the eastern and western Mediterranean regions and the higher influence of the North Atlantic dynamics in the western Mediterranean

The History of the El Niño - Southern Oscillation according to lacustrine and marine sediments

El gran impacte que El Niño — Oscil·lació del Sud (ENSO) té en la nostra societat industrialitzada ha esperonat la comunitat científica d'arreu a entendre quins són els mecanismes físics que el controlen, així com clarificar quina ha estat la seva història. El registre sedimentari de sensors naturals, com els llacs o la mar, ha permès reconstruir la història de l'ENSO. En aquest article, els autors donen una visió sintètica de la història d'aquest fenomen climàtic al llarg dels darrers quatre milions d'anys.The large impact of the El Niño – Southern Oscillation (ENSO) in our industrial society has spurred the scientific community to understand the physical processes that trigger this climate phenomenum and to elucidate its history. The sedimentary record of natural sensors, such as lakes and seas, was used to reconstruct the history of the ENSO and to obtain a comprehensive history of this climate phenomenon throughout the last 4 million years

Middle and late Holocene climate change and human impact inferred from diatoms, algae and aquatic macrophyte pollen in sediments from Lake Montcortès (NE Iberian Peninsula)

During the middle and late Holocene, the Iberian Peninsula underwent large climatic and hydrologic changes, but the temporal resolution and regional distribution of available palaeoenvironmental records is still insufficient for a comprehensive assessment of the regional variability. The high sedimentation rate in karstic, meromictic Montcortès Lake (Catalan pre-Pyrenees) allows for a detailed reconstruction of the regional palaeoecology over the last 5,340 years using diatom analysis, aquatic pollen, sedimentological data, and historic documentary records. Results show marked fluctuations in diatom species assemblage composition, mainly between dominant Cyclotella taxa and small Fragilariales. We suggest that the conspicuous alternation between Cyclotella comta and C. cyclopuncta reflects changes in trophic state, while the succession of centric and pennate species most likely reflects changes in the hydrology of the lake. The diatom assemblages were used to identify six main phases: (1) high productivity and likely lower lake levels before 2350 BC, (2) lower lake levels and a strong arid phase between 2350 and 1850 BC, (3) lake level increase between 1850 and 850 BC, (4) relatively high lake level with fluctuating conditions during the Iberian and Roman Epochs (650 BC–350 AD), (5) lower lake levels,unfavourable conditions for diatom preservation, eutrophication and erosion triggered by increased human activities in the watershed during the Medieval Climate Anomaly (900–1300 AD), and (6) relatively higher lake levels during the LIA (1380–1850 AD) and afterwards. The combined study of diatoms, algae and pollen provides a detailed reconstruction of past climate, which refines understanding of regional environmental variability and interactions between climate and socio-economic conditions in the Pyrenees.Financial support for this research was provided by the Spanish Inter-Ministry of Science and Technology (CICYT), through the projects LIMNOCLIBER (REN2003-09130-C02-02), LIMNOCAL (CGL2006-13327-C04-01) and GRACCIE-CONSOLIDER (CSD2007-00067). The Ebro Hydrographic Survey kindly provided updated, present-day limnological data. Two anonymous referees greatly improved a former version of this manuscript.Peer Reviewe