Divergência genética em feijoeiro em condições de inverno tropical

O objetivo deste trabalho foi avaliar a divergência genética de genitores de feijão tolerantes e não-tolerantes às condições de inverno e de suas combinações híbridas. A distância generalizada de Mahalanobis, o método de agrupamento de otimização de Tocher e a técnica de variáveis canônicas foram os procedimentos multivariados utilizados. Nos cruzamentos, utilizaram-se cultivares de feijão que se adaptam bem às condições de inverno, ou seja: Vermelho 2157, Ouro Negro, Antióquia 8 e Ricopardo 896, e as cultivares comerciais não-tolerantes, EMCAPA 404 -- Serrano, Carioca e EMCAPA 405 -- Goytacazes. Os genitores e as combinações híbridas nas gerações F1, F2 e F3 foram avaliados em Coimbra, Minas Gerais, em quatro ensaios, nos anos de 1995 e 1996. A divergência genética dos germoplasmas foi influenciada pela temperatura e pelo estádio de melhoramento. As cultivares mais dissimilares foram Antióquia 8 e EMCAPA 404 -- Serrano, e as mais similares foram, Ouro Negro e Ricopardo 896. O rendimento de grãos e o número de vagens por parcela apresentaram-se como as características de menor importância relativa no estudo da divergência genética. No entanto, como apresentaram baixa correlação genotípica com as demais características e eram as de maior importância no processo produtivo, não devem ser descartadas.

Mineralização de nitrogênio em solo tropical tratado com lodos de esgoto

A mineralização do N orgânico é um dos principais fatores que determinam as quantidades de lodos de esgoto (LE) a aplicar em solos. O objetivo deste trabalho foi quantificar, em laboratório, o potencial de mineralização de N orgânico num Latossolo Vermelho distroférrico, tratado com dois LE anaeróbios, um de origem estritamente urbana (Franca, SP) e outro com presença de despejos industriais (Barueri, SP). Os LE foram aplicados ao solo em doses de 1,5, 3, 6 e 12 g kg-1 (Franca) e 4, 8, 16 e 32 g kg-1 (Barueri), e o tempo de incubação foi de 15 semanas. O acúmulo de N inorgânico no solo ao final da incubação foi proporcional às quantidades de N orgânico adicionadas. O potencial de mineralização estimado pelo modelo exponencial simples foi de 24 mg kg-1 de N no solo sem lodo, e variou entre 44 e 265 mg kg-1 de N no solo tratado com os lodos. A fração de mineralização potencial do N orgânico dos lodos foi estimada em 31%. A mineralização foi mais lenta no solo tratado com as duas maiores doses do LE de Barueri. Os dois lodos acidificaram o solo; o de Franca causou acidificação mais intensa que o de Barueri.

Agrupamento de espécies arbóreas de uma floresta tropical por características de solo

A competição por nutrientes é um dos principais fatores que regulam tamanho e distribuição das populações arbóreas nos ecossistemas florestais da Amazônia, dada sua escassez na maioria dos solos da região. O objetivo deste trabalho foi agrupar parte das espécies arbóreas de uma floresta, por meio das características do solo. Foram utilizados dados de 32 espécies mais abundantes, distribuídas em 240 subparcelas de 10x10 m, localizadas em 12 parcelas de 1 ha, aleatoriamente demarcadas em uma floresta primária do Estado do Amapá, Amazônia Oriental. De acordo com técnicas de análises multivariadas, separaram-se as espécies em três grupos, que ocuparam diferentes faixas de variáveis químicas e texturais de solo. As variáveis de solo mais importantes na separação dos grupos foram Ca, Mg, K e Al. As espécies da família Melastomataceae concentraram suas populações em condições relacionadas a indicadores de menor fertilidade do solo. Os resultados sugerem que o substrato exerce papel importante no tamanho e na distribuição das populações arbóreas na floresta primária estudada.

Mixing of Rhône River water in Lake Geneva (Switzerland-France) inferred from stable hydrogen and oxygen isotope profiles

Depth profiles were sampled at different locations throughout Lake Geneva on a monthly and seasonal basis over the course of 2 years and analysed for their stable hydrogen and oxygen isotope compositions. The isotopic compositions indicate an isotopic stratification in the metalimnion during summer and fall. This is related to mixing of Rhône River water, which in summer is dominated by snow and glacier melt waters, and lake water, with the latter having a homogenous isotopic composition. The observed interflow layer is 7-15 m thick and can be traced by the distinct stable isotope composition of the water for about 55 km throughout the lake as well as into shallow bay regions. Depth of the interflow layer close to the Rhône River mouth is similar to those previously described based on echo-soundings and turbidity profiles of sediment dispersion. In contrast to previous descriptions of the interflow within Lake Geneva, the stable isotope compositions allow for direct, natural tracing of the Rhône River water even in cases where the turbidity and conductivity measurements do not indicate such an interflow. In addition, the method allows for a quantification of the Rhône River and lake water in the interflow with the fraction of Rhône River water within the interflow estimated to be up to 37% in summer. The isotopic composition further indicates different vertical mixing processes within the two lake basins of Lake Geneva, related to the density gradients and local stability within the water column. The method may be applicable to other lakes in catchments with large differences in the topography as water that originates from high altitudes or glaciers has a distinct oxygen and hydrogen isotope composition compared to other sources of water originating at lower altitudes and/or from direct precipitation over the lake. Stable isotope measurements thus improve the understanding of the circulation of water within the lake, which is fundamental for an evaluation of the water residence times, dissolved pollutant and nutrient transport as well as oxygenation.

Iowa Historic Property Study: Iowa-Illinois Memorial Bridge Carrying I-74 and U.S. 6 over Mississippi River between Bettendorf, Scott County, Iowa and Moline, Rock Island County, Illinois, 2012

The 1935 Iowa-Illinois Memorial Bridge is being documented at this time to fulfill the requirements of the Memorandum of Agreement regarding the removal of the Iowa-Illinois Memorial Bridge and the Iowana Farms Milk Company Building for the proposed improvements to Interstate 7 4 in Bettendorf, Iowa, and Moline, Illinois.1 The 1959 twin suspension bridge will be removed as well, but it was determined to be ineligible for the National Register of Historic Places. Discussion of the history of the 1959 twin span is included, however, in the current report as part of the overall history of the Iowa-Illinois Memorial Bridge. Fieldwork for the documentation occurred in November 2009 and October 2010 (Fig. 1). Limitations on photography included limited shoreline access on the Illinois side, making good views of the bridge from the south somewhat challenging. Also, photographs on the bridge deck were not possible because of interstate traffic and prohibitions on pedestrian traffic. Within the last few years, online primary sources have proliferated, along with historical materials regarding the Iowa-Illinois Memorial Bridge. Sources available online for this report included numerous historical photographs, as well as historical Davenport, Iowa, and U.S. newspapers that document the bridge planning and construction. Additional primary source material was found at the University of Iowa Libraries, the State Historical Society of Iowa in Iowa City, the Bettendorf Public Library, the Richardson-Sloane Special Collections Center at the Davenport Public Library, and the Iowa State University Special Collections in Ames.

Fish passage assessment at the most downstream barrier of the Ebro River (NE Iberian Peninsula)

Fish passage at artificial barriers is necessary for the conservation of healthy fish stocks. The first barrier that migratory fish encounter when ascending the Ebro River is the Xerta Weir, where a pool-type fishway was constructed in 2008. From 2007 to 2010, boat electrofishing surveys were conducted in the Ebro River downstream of the Xerta Weir to assess the potential pool of species that could use the fishway. Nine native and 12 exotic species were captured, the latter comprising 62 % of the relative abundance and 70 % of the biomass. A combination of video recording, electrofishing and trapping was used to assess the effectiveness of the fishway in facilitating the passage of fish. Eight species were detected using the fishway, of which five were native (Liza ramada, Anguilla anguilla, Barbus graellsii, Gobio lozanoi and Salaria fluviatilis) and three exotic (Alburnus alburnus, Cyprinus carpio and Rutilus rutilus). Only L. ramada used the fishway in substantial numbers. The rate of fish passage was the highest from June to August and decreased afterwards. The effectiveness of the fishway might be lowered by areas of turbulence within the fishway and by distraction flows from a nearby hydropower station

Missouri River Studies: Alluvial Morphology and Engineering Soil Classification, HR-1, Progress Report, 1960

The primary purposes of this investigation are: 1) To delineate flood plain deposits with different geologic and engineering properties. 2) To provide basic data necessary for any attempt at stabilizing flood plain deposits. The alluvial valley of the Missouri River adjacent to Iowa was chosen as the logical place to begin this study. The river forms the western boundary of the state for an airline distance of approximately 139 miles; and the flood plain varies from a maximum width of approximately 18 miles (Plates 2 and 3, Sheets 75 and 75L) to approximately 4 miles near Crescent, Iowa (Plate 8, Sheet 66). The area studied includes parts of Woodbury, Monona, Harrison, Pottawattamie, Mills, and Fremont counties in Iowa and parts of Dakota, Thurston, Burt, Washington, Douglas, Sarpy, Cass and Otoe counties in Nebraska. Plate l is an index map of the area under consideration.

Diverging Cave- and River-Dwelling Newts Exert the Same Mate Preference in their Native Light Conditions

When colonizing a new habitat, populations must adapt their sexual behaviour to new ecological constraints. Because caves display drastically different conditions from surface habitats and cave animals are deprived from visual information, hypogean populations are expected to have modified their mate preference and signalling behaviour after cave colonization. Here, we experimentally examined the female preference and the sexual behaviour of brook newts Calotriton asper from different cave and river populations, either in light or in darkness. Our results suggest that females prefer large individuals in both hypogean and epigean populations, but that this preference is only expressed in the light conditions of their native habitat. Hence, some mate choice criteria would be maintained across genetically divergent populations and throughout dissimilar habitats. However, this sexual behaviour is likely to be expressed via a different sensory pathway in the different habitats, suggesting that a sensory shift has occurred in cave populations, enabling animals to communicate through a non-visual channel.

The ager tarraconensis project (right side of river Francoli) (PAT): the application of geophysical survey to identify rural Roman settlement typologies

The methodology of the ager Tarraconensis project also included geophysical surveys aiming to distinguish different categories of rural settlements. Two geophysical techniques (resistivity and magnetometry) were combined to reveal traces of unearth structures from a selection of sites identified from the field survey. Results of geophysical surveys of these seven sites as well as conclusions obtained from this approach are discussed here.

Audit report on the Great River Regional Waste Authority for the year ended June 30, 2014

Audit report on the Great River Regional Waste Authority for the year ended June 30, 2014

A new spin on a compositionalist predictive modelling framework for conservation planning: a tropical case study in Ecuador

Knowledge about spatial biodiversity patterns is a basic criterion for reserve network design. Although herbarium collections hold large quantities of information, the data are often scattered and cannot supply complete spatial coverage. Alternatively, herbarium data can be used to fit species distribution models and their predictions can be used to provide complete spatial coverage and derive species richness maps. Here, we build on previous effort to propose an improved compositionalist framework for using species distribution models to better inform conservation management. We illustrate the approach with models fitted with six different methods and combined using an ensemble approach for 408 plant species in a tropical and megadiverse country (Ecuador). As a complementary view to the traditional richness hotspots methodology, consisting of a simple stacking of species distribution maps, the compositionalist modelling approach used here combines separate predictions for different pools of species to identify areas of alternative suitability for conservation. Our results show that the compositionalist approach better captures the established protected areas than the traditional richness hotspots strategies and allows the identification of areas in Ecuador that would optimally complement the current protection network. Further studies should aim at refining the approach with more groups and additional species information.

Organic matter processing and soil evolution in a braided river system

Traditionally, braided river research has considered flow, sediment transport processes and, recently, vegetation dynamics in relation to river morphodynamics. However, if considering the development of woody vegetated patches over a time scale of decades, we must consider the extent to which soil forming processes, particularly related to soil organic matter, impact the alluvial geomorphic-vegetation system. Here we quantify the soil organic matter processing (humification) that occurs on young alluvial landforms. We sampled different geomorphic units, ranging from the active river channel to established river terraces in a braided river system. For each geomorphic unit, soil pits were used to sample sediment/soil layers that were analysed in terms of grain size (<2mm) and organic matter quantity and quality (RockEval method). A principal components analysis was used to identify patterns in the dataset. Results suggest that during the succession from bare river gravels to a terrace soil, there is a transition from small amounts of external organic matter supply provided by sedimentation processes (e.g. organic matter transported in suspension and deposited on bars), to large amounts of autogenic in situ organic matter production due to plant colonisation. This appears to change the time scale and pathways of alluvial succession (bio-geomorphic succession). However, this process is complicated by: the ongoing possibility of local sedimentation, which can serve to isolate surface layers via aggradation from the exogenic supply; and erosion which tends to create fresh deposits upon which organic matter processing must re-start. The result is a complex pattern of organic matter states as well as a general lack of any clear chronosequence within the active river corridor. This state reflects the continual battle between deposition events that can isolate organic matter from the surface, erosion events that can destroy accumulating organic matter and the early ecosystem processes necessary to assist the co-evolution of soil and vegetation. A key question emerges over the extent to which the fresh organic matter deposited in the active zone is capable of significantly transforming the local geochemical environment sufficiently to accelerate soil development.

Floods of June 17, 1990 and July 9, 1993, Along Squaw Creek and the South Skunk River in Ames, Iowa, and Vicinity, HR-140, 1996

Water-surface-elevation profiles and peak discharges for the floods of June 17, 1990, and July 9, 1993, along Squaw Creek and the South Skunk River, in Ames, Iowa, are presented in this report. The maximum flood-peak discharge of 24,300 cubic feet per second for the streamflow-gaging station on Squaw Creek at Ames, Iowa (station number 05470500) occurred on July 9, 1993. This discharge was 80 percent larger than the 100-year recurrence-interval discharge and exceeded the previous record flood-peak discharge of June 17, 1990, by 94 percent. The July 9, 1993, flood-peak discharge of 26,500 cubic feet per second on the South Skunk River below Squaw Creek (station number 05471000) was also a peak of record, exceeding the previous record flood-peak discharge of June 27,1975, by 80 percent, and the 100-year recurrence-interval discharge by 60 percent. A flood history describes rainfall conditions for floods that occurred during 1990 and 1993.

Manejo do nitrogênio para eficiência de uso por cultivares de feijoeiro em várzea tropical

O objetivo deste trabalho foi avaliar a resposta e a eficiência do uso de N, por cultivares de feijoeiro, em função do manejo do fertilizante nitrogenado em solo de várzea. O delineamento experimental foi o inteiramente casualizado, com seis repetições, no esquema de parcelas divididas constituídas pelos manejos de N, e as subparcelas pelas cultivares. A aplicação de N no sulco de semeadura causou efeito salino do fertilizante, o que reduziu a população de feijoeiros. A incorporação de todo o N em sulcos distintos das linhas da semeadura, por ocasião dessa ou até 15 dias após a emergência, é mais eficaz no aumento da produtividade de grãos de feijão, do que a aplicação a lanço na superfície ou incorporada com grade antes da semeadura. A cultivar BRS Pontal foi a mais produtiva, o que é indicativo de alta adaptação ao ambiente de várzea tropical. Houve diversidade na eficiência de uso de N entre as cultivares de feijoeiro, e as de ciclo médio foram mais eficientes do que as precoces. A produtividade de grãos foi positivamente associada às eficiências agronômica, de recuperação e de utilização de N. A produtividade de grãos e a eficiência de uso de N pelas cultivares diferem conforme o manejo do fertilizante nitrogenado.