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Measurements and modelling of evapotranspiration to assess agricultural water productivity in basins with changing land use patterns: a case study in the Sao Francisco River basin, Brazil.

机译:蒸散量的测量和建模,以评估土地利用方式不断变化的流域的农业水生产率:以巴西圣弗朗西斯科流域为例。

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摘要

The São Francisco River basin in Brazil is marked by socio-economic disparities and environrnental vulnerabilities. Water managers in the semi-arid region of the basin are faced with several challenges, such as competition among different water user groups, local over-exploitation of aquifers, c1imateand land use changes, non-source pollution, erosion, and sedimentation. Water policy makers have to work out strategies for integrated water management, which rely on a proper knowledge base of the physical conditions encountered in the basin. The intensification of horticulture in the semi-arid north-eastem region of Brazil replaces natural vegetation (i.e. caatinga) by irrigated fruit crops. A proper knowledge of the water balance from these different agro-ecosystems is an essential pre-requisite for sound water resources planning in the basin context. Because of the importance of agricultural water management practices on basin hydrology, daily and seasonal actualK.nowledge of spatially variable actual evapotranspiration can help to optimize the necessary reduction in irrigation supplies.evapotranspiration were measured in irrigated crops, along with experimental data collection over caatinga. Advanced radiation andenergy balance measurements were conducted using the Bowen ratio and eddy correlation energy balance methods. Remote sensing algorithms are potentially suitable for the extrapolation of these local fluxes on a regional scale, and the opportunities of these tools were investigated. The key crop water parameters identified from this data set inc1uded actual evapotranspiration, actual transpiration, actual soil evaporation, evaporative fractions, aerodynamic resistances, surface resistances, crop coefficients, percolation fluxes and water productivity.The energy balance measurements on the irrigated fields revealed high evaporative fractions, which pointed out that soils are very wet and that large majority of the net available energy is converted into latent heat fluxoThe average crop water consumption in wine grape were found to be 478 mm per growing season, while table grapes show 373 mm per growing season. The seasonal accumulated values for mango orchardswere typical1y 1419 mm. On average the caatinga natural ecosystem evapotranspirated only 533 mm yr-I. The irrigation induced an incremental evapotranspiration of 2.2 mm d-I or 8,030 m3 ha-I yr-I. The water balances revealed that systematic over-irrigation is a common practice and that a continuous deep percolation flux occurs. The detailed results allowed expressing water consumption into specific bio-physical parameters, rather than only into more generic crop coefficients that lump together several individual crop water parameters. The stomata o irrigated crops seem to respond very tight1y to atmospheric vapour pressure deficit while natural vegetation responds to the rainfall regime. The field results have been used further to calibrate and validate an existing remote sensing algorithm for the estimation of spatially distributed energy balance fluxes: the Surface Energy Balance AIgoritlun for Land (SEBAL). It was shown that it is required to apply the hot and cold pixel calibration for every individual image. A generic solution for the internal calibration of the sensible heat flux through the linear relationship between surface radiation temperature and vertical air temperature differences adjacent to the land surface could not be found. For daily scale, the values of the instantaneous evaporative fraction needed to be adjusted. The difference between field measurements and SEBAL was 4.4 % and 0.6% for natural vegetation and irrigated mango orchard, respectively, for annual scale. Further to the estimate of depleted water volumes in irrigated horticulture, it was investigated whether the incremental evapotranspiration values are productive. After calibration, the SEBAL algorithm was applied to determine regional scale evapotranspiration and biomass production. The remote sensing tools shows spatial variation of crop water productivity values and detects regions and farms where water can be saved. The net water withdrawal in the Low-Middle São Francisco River basin was also estimated. The biophysical water productivity based on actual evapotranspiration appeared to be around 0.90 L m-3,2.80 kg m-3and 3.4 kg m-3for respectively wine grapes, table grapes, and mangos. The economic water productivities indicated that irrigated fruit crops have around 20 times more value per unit water consumed than irrigated arable crops. The area with fruit crops in the semi-arid region of the Low-Middle São Francisco River basin are expanding mainly with vineyards and mango orchards. The crop water consumption is high due to overirrigation together with high thermal availability. The water is, however, productively used and creates a boost for the rural economy. The drawback is that agricultural drainage can adversely affect the water quality, and this requires a lower irrigation supply in the near-future. K.nowledge of spatially variable actual evapotranspiration can help to optimize the necessary reduction in irrigation supplies.
机译:巴西的圣弗朗西斯科河流域的特点是社会经济差异和环境脆弱性。流域半干旱地区的水资源管理者面临着若干挑战,例如不同用水户群体之间的竞争,含水层的局部过度开发,土地利用和土地利用变化,无源污染,侵蚀和沉积。水政策制定者必须制定综合水管理战略,这要依靠对流域遇到的自然条件的适当了解。巴西半干旱东北地区的园艺集约化利用灌溉的水果作物代替了自然植被(即caatinga)。对这些不同的农业生态系统的水平衡有适当的了解,是在流域范围内合理规划水资源的必要先决条件。由于农业用水管理实践对流域水文学的重要性,因此,了解每日和季节性的实际K蒸散知识有助于优化必要的灌溉量减少。对灌溉作物的蒸散量进行了测量,并收集了Caatinga上的实验数据。使用鲍文比和涡旋相关能量平衡方法进行了先进的辐射和能量平衡测量。遥感算法可能适合在区域范围内外推这些局部通量,并研究了这些工具的机会。从该数据集中确定的关键作物水分参数包括实际蒸散量,实际蒸腾量,实际土壤蒸发量,蒸发分数,空气动力学阻力,表面阻力,作物系数,渗透通量和水分生产率。灌溉田地的能量平衡测量显示出高蒸发量分数表明土壤非常湿,大部分净可用能量转化为潜热通量。酿酒葡萄的平均作物耗水量为每个生长期478毫米,而鲜食葡萄则为373毫米季节。芒果园的季节累积值通常为1419毫米。平均而言,caatinga自然生态系统的蒸散量仅为533 mm yr-I。灌溉引起的蒸散量增加了2.2 mm d-I或8,030 m3 ha-I yr-I。水平衡表明,系统性过度灌溉是一种普遍做法,并且会发生连续的深层渗流。详细的结果允许将耗水量表达为特定的生物物理参数,而不是仅表达为将几个单独的作物水分参数汇总在一起的更通用的作物系数。灌溉作物的气孔似乎对大气蒸气压亏缺反应非常紧,而自然植被对降雨状况做出响应。现场结果已被进一步用于校准和验证现有的遥感算法,用于估算空间分布的能量平衡通量:地面能量平衡AIgoritlun for Land(SEBAL)。结果表明,需要对每个单独的图像应用冷像素校准。找不到通过表面辐射温度与邻近陆地表面的垂直空气温度差之间的线性关系对显热通量进行内部校准的通用解决方案。对于日刻度,需要调整瞬时蒸发分数的值。年度规模的自然植被和灌溉芒果园的实地测量值与SEBAL之间的差异分别为4.4%和0.6%。除了估算灌溉园艺中的枯竭水量外,还研究了增加的蒸散量是否具有生产力。校准后,将SEBAL算法应用于确定区域规模的蒸散量和生物量生产。遥感工具显示了作物水分生产率值的空间变化,并检测了可以节水的地区和农场。还估计了圣弗朗西斯科州中低流域的净取水量。酿酒葡萄,食用葡萄和芒果的实际蒸发蒸腾量的生物物理水生产率分别约为0.90 L m-3、2.80 kg m-3和3.4 kg m-3。经济用水生产率表明,灌溉的水果作物每单位水消耗的价值是灌溉的可耕作物的20倍左右。低中圣弗朗西斯科河流域的半干旱地区的水果作物面积主要是葡萄园和芒果园。由于过度灌溉和高热利用率,农作物耗水量很高。但是,水被大量使用,并为农村经济带来了动力。缺点是农业排水会对水质产生不利影响,这需要在不久的将来减少灌溉供应。了解空间上可变的实际蒸散量可以帮助优化灌溉供应量的必要减少。

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    TEIXEIRA A. H. de C.;

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  • 年度 2008
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