Regional drivers of clutch loss reveal important trade-offs for beach-nesting birds

Coastal birds are critical ecosystem constituents on sandy shores, yet are threatened by depressed reproductive success resulting from direct and indirect anthropogenic and natural pressures. Few studies examine clutch fate across the wide range of environments experienced by birds; instead, most focus at the small site scale. We examine survival of model shorebird clutches as an index of true clutch survival at a regional scale (∼200 km), encompassing a variety of geomorphologies, predator communities, and human use regimes in southeast Queensland, Australia. Of the 132 model nests deployed and monitored with cameras, 45 (34%) survived the experimental exposure period. Thirty-five (27%) were lost to flooding, 32 (24%) were depredated, nine (7%) buried by sand, seven (5%) destroyed by people, three (2%) failed by unknown causes, and one (1%) was destroyed by a dog. Clutch fate differed substantially among regions, particularly with respect to losses from flooding and predation. ‘Topographic’ exposure was the main driver of mortality of nests placed close to the drift line near the base of dunes, which were lost to waves (particularly during storms) and to a lesser extent depredation. Predators determined the fate of clutches not lost to waves, with the depredation probability largely influenced by region. Depredation probability declined as nests were backed by higher dunes and were placed closer to vegetation. This study emphasizes the scale at which clutch fate and survival varies within a regional context, the prominence of corvids as egg predators, the significant role of flooding as a source of nest loss, and the multiple trade-offs faced by beach-nesting birds and those that manage them.

A novel α-aminophosphonic acid-modified acrylamide-based hydrophobic associating copolymer with superb water solubility for enhanced oil recovery

As a non-renewable resource, the rational exploitation of oil has attracted a large amount of attention. Among many methods for enhanced oil recovery, polymer flooding is the most suitable method of chemical flooding for non-marine reservoirs and therefore various modified acrylamide-based copolymers have been studied. In this study, a novel α-aminophosphonic acid-modified hydrophobic associating copolymer was successfully synthesized by copolymerization of acrylamide, acrylic acid, N-allyldodecanamide and 1-(dimethylamino)allylphosphonic acid. The copolymer was characterized by FT-IR, 1H NMR and thermogravimetry and exhibited superior water solubility and thickening capability. Subsequently, the shear resistance, temperature resistance and salt tolerance of the copolymer solution were investigated. The value of apparent viscosity retention of a 2000 mg L-1 copolymer solution was as high as 58.55 mPa s at a shear rate of 170 s-1 and remained at 40.20 mPa s at 120 °C. The values of apparent viscosity retention of 55.41 mPa s, 59.95 mPa s and 52.97 mPa s were observed in solutions of 10000 mg L-1 NaCl, 1200 mg L-1 MgCl2, and 1200 mg L-1 CaCl2, respectively. These were better than those of partially hydrolyzed polyacrylamide under the same conditions. In addition, an increase of up to 14.52% in the oil recovery rate compared with that for water flooding could be achieved in a core flooding test using a 2000 mg L-1 copolymer solution at 65 °C.

SLOPE STABILITY ANALYSIS OF MOUNT MEAGER, SOUTH-WESTERN BRITISH COLUMBIA, CANADA

The Mount Meager Volcanic Complex (MMVC) in south-western British Columbia is a potentially active, hydrothermally altered massif comprising a series of steep, glaciated peaks. Climatic conditions and glacial retreat has led to the further weathering, exposure and de-buttressing of steep slopes composed of weak, unconsolidated material. This has resulted in an increased frequency of landslide events over the past few decades, many of which have dammed the rivers bordering the Complex. The breach of these debris dams presents a risk of flooding to the downstream communities. Preliminary mapping showed there are numerous sites around the Complex where future failure could occur. Some of these areas are currently undergoing progressive slope movement and display features to support this such as anti-scarps and tension cracks. The effect of water infiltration on stability was modelled using the Rocscience program Slide 6.0. The main site of focus was Mount Meager in the south- east of the Complex where the most recent landslide took place. Two profiles through Mount Meager were analysed along with one other location in the northern section of the MMVC, where instability had been detected. The lowest Factor of Safety (FOS) for each profile was displayed and an estimate of the volume which could be generated was deduced. A hazard map showing the inundation zones for various volumes of debris flows was created from simulations using LAHARZ. Results showed the massif is unstable, even before infiltration. Varying the amount of infiltration appears to have no significant impact on the FOS annually implying that small changes of any kind could also trigger failure. Further modelling could be done to assess the impact of infiltration over shorter time scales. The Slide models show the volume of material that could be delivered to the Lillooet River Valley to be of the order of 109 m3 which, based on the LAHARZ simulations, would completely inundate the valley and communities downstream. A major hazard of this is that the removal of such a large amount of material has the potential to trigger an explosive eruption of the geothermal system and renew volcanic activity. Although events of this size are infrequent, there is a significant risk to the communities downstream of the complex.

Influence of Habitat on the Reproductive Ecology of the Amazonian Palm, Mauritia flexuosa, in Roraima, Brazil

Although Mauritia flexuosa (Arecaceae) plays a pivotal role in the ecology and economy of the Amazon, and occurs in a variety of habitats, little is known about the influence of habitat on the reproductive biology of this palm. My dissertation focuses on the reproductive biology of M. flexuosa in three habitats in Roraima, Brazil: undisturbed forest, undisturbed forest-savanna ecotone, and savanna disturbed by plantations of the exotic tree, Acacia mangium. First, I calculated sex ratios and linked precipitation patterns with phenology. Sex ratios were female-biased. Precipitation was negatively associated with flowering, and positively associated with fruiting. Habitat appears to have no significant influence on phenology of M. flexuosa, although short-term climate variation may affect phenology of this species. Second, I examined floral biology, observed floral visitors, and performed exclusion experiments to determine the pollination system of M. flexuosa. Fruit set did not differ significantly between the visitor exclusion treatment and the control, but was significantly lowest in the wind + visitor exclusion treatment, suggesting that this dioecious palm is anemophilous, independent of habitat. Third, I identified the abiotic and biotic factors explaining variation in fruit mass, seed mass, seed number per fruit, and total fruit yield among habitats. Soil moisture and flooding during the wet season were the best predictors of fruit and seed output. The number of leaves, diameter at breast height, and height were all accurate predictors of reproductive output, but crown volume did not accurately predict fruit yields. Results re-evaluate traditional assumptions about wind-pollination in the tropics, and highlight abiotic and biotic factors responsible for variation in reproductive output of M. flexuosa, with implications for effective management of this palm. Finally, I interviewed harvesters and vendors to document the traditional knowledge and market dynamics of the fruit of M. flexuosa, buriti. Traditional knowledge corroborated results from scientific studies. Vendors argued that the price of buriti must increase, and must fluctuate with varying supply. With appropriate economic incentives to vendors/harvesters, Roraima may expand its market infrastructure for buriti, effectively stimulating the regional economy and practicing sustainable harvesting.

Analyzing Tidal Fluctuations in the Big Pine Key Freshwater Lens with Time-Lapse Resistivity

The tidal influence on the Big Pine Key saltwater/freshwater interface was analyzed using time-lapse electrical resistivity imaging and shallow well measurements. The transition zone at the saltwater/freshwater interface was measured over part of a tidal cycle along three profiles. The resistivity was converted to salinity by deriving a formation factor for the Miami Oolite. A SEAWAT model was created to attempt to recreate the field measurements and test previously established hydrogeologic parameters. The results imply that the tide only affects the groundwater within 20 to 30 m of the coast. The effect is small and caused by flooding from the high tide. The low relief of the island means this effect is very sensitive to small changes in the magnitude. The SEAWAT model proved to be insufficient in modeling this effect. The study suggests that the extent of flooding is the largest influence on the salinity of the groundwater.

Comparison and Validation of Tropical Rainfall Measuring Mission (TRMM) Rainfall Algorithms in Tropical Cyclones

Tropical Rainfall Measuring Mission (TRMM) rainfall retrieval algorithms are evaluated in tropical cyclones (TCs). Differences between the Precipitation Radar (PR) and TRMM Microwave Imager (TMI) retrievals are found to be related to the storm region (inner core vs. rainbands) and the convective nature of the precipitation as measured by radar reflectivity and ice scattering signature. In landfalling TCs, the algorithms perform differently depending on whether the rainfall is located over ocean, land, or coastal surfaces. Various statistical techniques are applied to quantify these differences and identify the discrepancies in rainfall detection and intensity. Ground validation is accomplished by comparing the landfalling storms over the Southeast US to the NEXRAD Multisensor Precipitation Estimates (MPE) Stage-IV product. Numerous recommendations are given to algorithm users and developers for applying and interpreting these algorithms in areas of heavy and widespread tropical rainfall such as tropical cyclones.

Review of Managing the Fraud Risk in the Disaster Supplemental Nutrition Assistance Program (D-SNAP), Administered by the Department of Social Services

This review was initiated based upon allegations from multiple sources of possible fraud in the Disaster Supplemental Nutrition Assistance Program (D-SNAP) administered by the South Carolina Department of Social Services (SCDSS), which was implemented in response to the 10/3/2015 statewide flooding from Hurricane Joaquin. This review’s scope and objectives were: Assess SCDSS’s D-SNAP implementation for compliance with federal guidelines, with emphasis on fraud preventative controls; Assess the SCDSS’s post-disaster review and audit methodology for compliance with federal guidelines, with emphasis on understanding the fraud risks and resolution strategies; and Identify residual risk/suspected fraud not addressed through the SCDSS review and available opportunities to address.

El agua como factor reordenador del territorio en el caso de las inundaciones de la Universidad de la Sabana en 2011

El objetivo de este estudio de caso es analizar el agua como factor reordenador del territorio, en el caso específico de las inundaciones sucedidas en el 2011 en el territorio de la Universidad de la Sabana. Durante la ola invernal del 2011 todo el país sufrió las consecuencias de los errores en la planeación de los asentamientos humanos. La no inclusión de la gestión del riesgo dentro del Ordenamiento Territorial, sumado la falta de comprensión de las dinámicas del territorio y del rol del agua como factor ordenador del territorio, causaron inundaciones y desastres naturales que afectaron la vida de miles de ciudadanos, entre eso los estudiantes, profesores y demás afectados por las inundaciones de la Universidad de la Sabana.

The flora and communities Carnaubal Palm Forest in the northern region of Ceará - Brazil

The “dicótilo-palmácea” mixed forest is found in the fluvial plains (floodplains) of watercourses on the Ceará semiarid region (Brazil), distinguishing from the surrounding vegetation (caatinga) by the prevalence of larger tree species. In the river’s margins, presenting high variability in the extension of the riverbanks, arise floodplains in pedologic complexes mainly composed by neossols and argissols, resulting from the deposition of sediments. In these areas of high fertility soils and subjected to flooding during part of the year, it develops a particular type of riparian vegetation dominated by carnauba palm tree (Copernicia prunifera (Mill.) H.E. Moore) forming a particular type of riparian forest, designated by carnaubal palm forest. We aimed to carry out floristic and phytosociological surveys of carnauba palm forests located in the northern region of Ceará. The classical sigmatist method of Braun-Blanquet was applied and classification analysis (Twinspan) was perfomed. The field work occurred in March 2014 and 2016 in eight areas: Fazenda Pedra Branca (03º 37’ 10’’ S e 40º 18’ 30’’ W, 104 m asl), Vale do Rio Bom Jesus (04º 04’ 42’’ S e 39º 57’ 08’’ W, 200 m asl), Lagoa do Peixe (03º 56’ 28’’ S e 40º 23’ 23’’ W, 97 m asl), Fazenda Peixes (04º 06’ 03’’ S e 40º 32’ 43’’ W, 114 m asl), Fazenda Natividade (04º 02’ 50’’ S e 40º 29’ 03’’ W, 109 m asl), Fazenda Morro Alto (02º 53’ 42’’ S e 39º 54’ 51’’ W, 16 m asl), Fazenda Araticum (03º 04’ 58’’ S e 40º 09’ 36’’ W, 19 m asl) and Fazenda Experimental da UVA (03º 37' 04'' S 40º 18' 18'' W, 200 m asl).The floristic list consists of 170 species, distributed between 127 genera and 50 families. Twenty-seven Brazilian endemic species were identified, from which 8 are exclusive of the Caatinga biome. The Fabaceae was the most representative family, with the highest number of species (28), followed by Poaceae (17), Malvaceaea (14), Euphorbiaceae (12), Asteraceaea (9), Convolvulaceae and Rubiaceae (9). The dominant life forms were therophytes (34%), phanerophytes (30%) and chamaephytes (18%). Two communities were identified as a result of the classification analysis using the Twinspan.

GENTES E INUNDACIONES EN LOS PUEBLOS DEL TEMPISQUE

Este artículo recoge la opinión de los habitantes de algunos de los pueblos ubicados en las tierras bajas de la cuenca del Tempisque, en relación con las dificultades que cada año enfrentan debido al desbordamiento de los ríos Tempisque y Las Palmas.ABSTRACT This article takes different opinions from the people living on the villages located in the lowlands of the Tempisque basin, related to the problems yearly they confront because of the Tempisque or Las Palmas rivers flooding.

PREVENCIÓN Y RESOLUCIÓN DE POTENCIALES CONFLICTOS SOCIOAMBIENTALES EN LA CUENCA DEL RÍO TÉRRABA: EL CASO DEL PROYECTO HIDROELÉCTRICO BORUCA

La microcuenca del río Poás (ubicada entre el volcán Barva y el volcán Poás, hasta la confluencia con el río Grande cerca de la ciudad de Alajuela) posee un alto potencial para la formación de acuíferos de alta calidad. Por este motivo sus recursos naturales deben utilizarse adecuadamente. La mejor manera de lograr lo anterior es mediante la planificación del uso de la tierra. En esta investigación se plantea para ello el ordenamiento territorial y el manejo de cuencas. Para este propósito se realiza una zonificación mediante la cual se identifican las siguientes zonas: sin restricción de uso, uso restringido y uso muy restringido. La mayor parte de la m icrocuenca (64,6%) se encuentra en la categoría de “sin restricción de uso”. Sin embargo. se hace necesaria la intervención con rapidez en sectores ubicados en la parte alta de la microcuenca que se clasifican de “uso muy restringido”. En relación con el recurso hídrico, en la microcuenca en los últimos 14 años y de acuerdo con la metodología aplicada, se ha elevado la producción hídrica, específicamente en la escorrentía y la ganancia. En general aumentó en 1,6%.Abstract:The Poas river micro watershed (located between the Barva and Poas volcanoes reaching the confluence of the Grande river near the city of Alajuela) has high potential for developing high quality aquifers, thus, its natural resnurces should be utilized adequately. This is best done by proper land use planning. In this study guidelines are presented for land use planning and watershed management. Land use is zoned or classified for the following uses:unrestricted use, restricted use, and highly restricted use. Most of the micro watershed (64.6 percent) is classified or zoned as ‘unrestricted use.’ However, urgent intervention is needed in demand and the possibility to export it. However, it is also possible to see the negative impaci of the project, such as: indigenous territories and a pan of the Interamerican Road being flooding, population displacement and the environmental ¡mpact on the Terraba-Sierpe mangrove. This diversity and incompatibility of factors and interest make a complex scenario that potentializes diverse conflicts.

SENSORES REMOTOS FOTOGRÁFICOS: ZONIFICACIÓN POR INUNDACIONES EN LAS CUENCAS BAJAS DE LOS RÍOS PARRITA Y LIMONCITO: UNA CARACTERIZACIÓN SOCIOESPACIAL MEDIANTE FOTOS AEREAS Y MAPAS

Usando procedimientos de trabajo con fotos aéreas de diferentes años, se analiza en el caso de la ciudad de Limón el avance del poblamiento hacia áreas costeras sujetas a inundaciones. Una vez diseñado el mapa que muestra para cuatro períodos la información extraída de las fotos aéreas, se realiza-un análisis físico –social de las condiciones  que dan origen a la vulnerabilidad al riesgo por inundación. En el caso del poblado de Parrita, se reconstruyen con ayuda de fotos aéreas, los distintos cursos fluviales que el río Parrita ha formado en un período de toma fotográfica aérea para cuatro años diferentes. Una vez dibujado este documento, se efectúa un análisis sobre las áreas de mayor riesgo por inundaciones, evaluando los aspectos sociales y económicos de la población afectada.  SUMMARY Using aerial photographs of different years, we analyze in the case of the Limon city, the growth population in coastal areas affected by flooding. A map showing four periods of aerial photointerpretation, fieldwork and another sources, gives information about the physical and social conditions of some areas with vulnerability by flooding. In the case of Parrita town, the use of aerial photographs of four periods, make it possible to know the geomorphological dynamic of Parrita river. With this map, we evaluate the risk by flooding, taking into account the social and economical aspects of the affected population.

DESLAZAMIENTOS EN LA CUENCA DEL RIO BANANO, UNA CONSECUENCIA DEL TERREMOTO DE ABRIL DE 1991

En la región Caribe algunas cuencas se vieron afectadas en su comportamiento hidrológico, como consecuencia del terremoto de abril de 1991.Un ejemplo evidente de lo anterior es la cuenca del rio Banano, que es la fuente principal del agua potable para la provincia de Limón, y que se presenta un comportamiento de rio aluvial acelerado como consecuencia de cerca de 40 millones de m3 de material deslizado. Los deslizamientos  característicos en la cuenca son deslizamientos de roca (rockslide), aunque puede observarse uno de tipo rotacional (rotational slump); además existen flujos de detritos ( debris flow). Este comportamiento acelerado origina inundaciones en poblados como Aguas Zarcas, Quitaría, Beverly; Polonia, Bomba y María Luisa. Con el fin de minimizar las consecuencias de estas inundaciones se establece una zonificación de áreas inundables para la parte baja de la cuenca en tres clases. Además, en la cuenca se registra un aporte significativo de material en suspensión, lo cual podrá alterar la posibilidad del agua. ABSTRACTThe April 1991 earthquake in Costa Rica caused changes in the hydrological characteristics of several watersheds in the Caribbean region of country.Evidence of these changes was observer in the rio Banano, the principal source of potable water for the province de Limon. The behavior of the alluvial river accelerated as a consequence of nearly 40 million cubic meters of material that moved within the watershed as a result of the earthquake. The characteristical landslides were rockslides, althoung rotational slump and debris flow slides were also observed. The accelerated hydrological changes in the river have caused flooding in populated areas such as Aguas Zarcas, Quitará, Beverly, Polonia, Bomba and Maria Luisa. In order to minimize the consequences of the flooding, the lower part of the watershed was classified in three categories according to flooding susceptibility.The river has also shown an increase in suspended material, which could affect the potability of the water.

LA ZONIFICACIÓN DE AMENAZA POR INUNDACIÓN COMO HERRAMIENTA PARA EL ORDENAMIENTO TERRITORIAL EN EL VALLE DEL RÍO SIXAOLA

En el caso de Costa Rica, uno de los eventos naturales que reviste especial importancia por su  frecuencia y daños acumulativos son las inundaciones; una herramienta para reducir los constantes desastres es la zonificación de amenazas por inundación. Mediante esta técnica es posible orientar el ordenamiento territorial y facilitar la gestión del riesgo. La cuenca del río Sixaola es una de las más afectadas por inundaciones en Costa Rica, en la parte baja se ubican asentamientos humanos habitados principalmente por núcleos de población altamente vulnerables. En este artículo se presenta la zonificación de amenaza por inundación, elaborada para el río Sixaola. ABSTRACT In the case of Costa Rica, one of the natural events of particular importance because of its frequency and cumulative damage is flooding. A tool to reduce this ongoing disaster is flood hazard zoning. Using this technique it is possible to guide land use planning and facilitate risk management. The Sixaola River Basin is one of the most affected by flooding in Costa Rica, and inhabitants of villages in the lower settlements are highly vulnerable. This article presents the flood hazard zoning plan developed for the Sixaola River.

Root behavior of savanna species in Brazil's Pantanal wetland.

The objective of this study was to determine the maximum depth, structure, diameter and biomass of the roots of common woody species in two savanna physiognomies (savanna woodland and open woody savanna) in Brazil's Pantanal wetland. The root systems of 37 trees and 34 shrubs of 15 savanna species were excavated to measure their length and depth and estimate the total root biomass through allometric relationships with stem diameter at ground level. In general, statistical regression models between root weight and stem diameter at ground level showed a significance of P < 0.05 and R2 values close to or above 0.8. The average depths of the root system in wetland savanna woodland and open woody savanna are 0.8 ± 0.3 m and 0.7 ± 0.2 m, respectively, and differ from the root systems of savanna woody species in non-flooding areas, whose depth usually ranges from 3 to 19 m.Weattribute this difference to the adaptation of woody plant to the shallow water table, particularly during the wet season. This singularity of woody species in wetland savannas is important when considering biomass and carbon stocks for national and global carbon inventories.