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Hydrological trade-offs due to different land covers and land uses in the Brazilian Cerrado

机译:巴西塞拉多地区不同的土地覆盖和土地用途导致的水文权衡

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Farmland expansion in the Brazilian Cerrado, considered one of the largest agricultural frontiers in the world, has the potential to alter water fluxes on different spatial scales. Despite some large-scale studies being developed, there are still few investigations in experimental sites in this region. Here, we investigate the water balance components in experimental plots and the groundwater table fluctuation in different land covers: wooded Cerrado, sugarcane, pasture and bare soil. Furthermore, we identify possible water balance trade-offs due to the different land covers. This study was developed between 2012 and 2016 in the central region of the state of S?o Paulo in southern Brazil. Hydrometeorological variables, groundwater table, surface runoff and other water balance components were monitored inside experimental plots containing different land covers; the datasets were analyzed using statistical parameters; and the water balance components uncertainties were computed. Replacing wooded Cerrado by pastureland and sugarcane shifts the overland flow (up to 42?mm?yr sup?1/sup ) and the water balance residual (up to 504?mm?yr sup?1/sup ) and may affect groundwater table behavior. This fact suggests significant changes in the water partitioning in a transient land cover and land use (LCLU) system, as the evapotranspiration is lower (up to 719?mm?yr sup?1/sup ) in agricultural land covers than in the undisturbed Cerrado. We recommend long-term observations for continuing the evaluations initiated in this study, mainly because there are few basic studies on tropical environments at the hillslope scale and more assessments are needed for a better understanding of the real field conditions. Such efforts should be made to reduce uncertainties, validate the water balance hypothesis and catch the variability of hydrological processes.
机译:被认为是世界上最大的农业疆域之一的巴西塞拉多的农田扩张有潜力在不同的空间尺度上改变水通量。尽管正在进行一些大规模的研究,但是在该地区的实验点上仍然很少进行研究。在这里,我们调查了实验地块中的水平衡成分以及不同土地覆被(树木繁茂的塞拉多,甘蔗,牧场和裸露的土地)的地下水位波动。此外,我们确定了由于土地覆盖范围不同而可能实现的水平衡权衡。该研究于2012年至2016年之间在巴西南部圣保罗州的中部地区进行。在包含不同土地覆盖的试验区内监测水文气象变量,地下水位,地表径流和其他水平衡要素;使用统计参数分析数据集;并计算了水平衡成分的不确定性。用牧场和甘蔗代替树木繁茂的塞拉多,改变了陆上水流(最高42?mm?yr ?1 )和剩余水平衡(最高504?mm?yr ?1 ),并可能影响地下水位行为。这一事实表明,在瞬时土地覆盖和土地利用(LCLU)系统中,水的分配发生了显着变化,因为农业土地覆盖的蒸散量比最高(最高719?mm?yr ?1 )低。在不受干扰的塞拉多。我们建议您进行长期观察,以继续进行此研究中的评估,这主要是因为在坡度尺度上对热带环境的基础研究很少,并且需要更多评估才能更好地了解实际田间条件。应该做出这样的努力以减少不确定性,验证水平衡假设并掌握水文过程的可变性。

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