O objetivo deste trabalho foi o de avaliar a seletividade da mistura de oxyfluorfen e ametryne, a dez cultivares de cana-de-açúcar. Utilizou-se as doses de 0,48 e 1,5 kg de i.a. / ha (2,0 e 3,0 l de p.c./ha), respectivamente. As cultivares utilizadas foram: RB 83-5089, RB 80-6043, RB 78-5148, RB 82-5336, RB 83-5486, RB 72-454, SP 79- 1011, SP 70-1143, SP 71-1406 e SP 80-1842. Os herbicidas, em mistura de tanque, foram aplicados em pré ou pós-emergência (5 e 29 dias após o plantio, respectivamente). As testemunhas de cada variedade foram capinadas manualmente. O plantio foi feito nos dias 24 e 25 /03/94. Nas parcelas com aplicação em préemergência verificou-se sintomas de intoxicação (avermelhamento e necrose) em 4,72% (RB 83-5089) a 14,58% (RB 82-5336) da área foliar da cultura; em pós-emergência os sintomas alcançaram entre 20,16% (SP 71-1406) e 45,44% (80-1842) da área foliar da cana. Com o crescimento da planta (a partir da oitava folha definitiva), as novas folhas emitidas não apresentaram sintomas de intoxicação. Não foram verificados efeitos dos herbicidas sobre o crescimento (emissão de folhas e altura das plantas), perfilhamento, produtividade e características tecnológicas dos colmos obtidos.
High-mountain basins provide a source of valuable water resources. This paper presents hydrological models for the evaluation of water resources in the highmountain Zêzere river basin in Serra da Estrela, Central Portugal. Models are solved with VISUAL BALAN v2.0, a code which performs daily water balances in the root zone, the unsaturated zone and the aquifer and requires a small number of parameters. A lumped hydrological model fails to fit measured stream flows. Its limitations are overcome by considering the dependence of the temperature and precipitation data with elevation and the spatial variability in hydrogeomorphological variables with nine sub-basins of uniform parameters. Model parameters are calibrated by fitting stream flow measurements in the Zêzere river. Computed stream flows are highly sensitive to soil thickness, whereas computed groundwater recharge is most sensitive to the interflow and percolation recession coefficients. Interflow is the main component of total runoff, ranging from 41 to 55% of annual precipitation. High interflows are favored by the steep relief of the basin, by the presence of a high permeability soil overlying the fractured low permeability granitic bedrock and by the extensive subhorizontal fracturing at shallow depths. Mean annual groundwater recharge ranges from 11 to 15% of annual precipitation. It has a significant uncertainty due to uncertainties in soil parameters. This methodology proves to be useful to handle the research difficulties regarding a complex mountain basin in a context of data scarcity.
The Ferraria thermal water emerges at the sea level in the Ferraria lava delta (western edge of S. Miguel Island, Azores) with temperature of ca. 60°C and pH varying between 5.4 and 6.2. It is of sodium chloride type, resulting from ca. 50% seawater mixing with an acid brackish, at &100°C, denoting the presence of significant CO 2 (g) and the progress of water-rock interactions in open system conditions. The thermal Na-Cl water is strongly enriched with Sr and Mn and, comparatively, has low concentrations in Al, Fe and As. These elements are removed from the solution as critical conditions for the formation of several neo-formed mineral phases are gradually attained. Thermodynamic equilibrium calculations are consistent with this interpretation, showing that the thermal fluid can precipitate Fe 3? -(hydr-)oxides, kaolinite and noncrystalline silica. Wells logging show fracture planes and pores fully/partly filled up with polyphase botryoidal aggregates mostly composed of goethite ? ferrihydrite and displaying variable adsorbed contents of Si, P and As. These neo-formed phases result from the pristine fluid oxidation due to seawater mixing; its precipitation is easily affected by pH and redox variations of the brackish, due to volcanic gases pressure alterations, and fluid pressure or flowvelocity oscillation in the fractured aquifer.
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