首页> 外文OA文献 >Soil water content variations and hydrological relations of the cropland-treebelt-desert land use pattern in an oasis-desert ecotone of the Heihe River Basin, China
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Soil water content variations and hydrological relations of the cropland-treebelt-desert land use pattern in an oasis-desert ecotone of the Heihe River Basin, China

机译:黑河流域绿洲荒漠过渡带退耕还林还草模式的土壤水分变化与水文关系。

摘要

This study considered the croplarid-treebelt-desert system in the arid inland river basin as an entire continuum to investigate the soil water content variation and hydrological relation. For this objective, the volumetric soil water content and plant root distribution was measured to 300 cm depth along a cropland-treebelt-desert site at the oasis-desert ecotone in the Heihe River Basin, China. The results showed that the mean soil water content in the 0-200 cm layer was greater in the cropland (8.88%) than that in the treebelt (5.78%) and desert (4.37%) as a result of frequent irrigation events. However, the cropland had noticeably lower mean soil water content below 200 cm depth (14.27%), compared to treebelt (18.07%) and desert (17.30%) with deeper roots to suck up groundwater. The decline process in soil water content pulse of the cropland and treebelt after irrigation event could be well described by an exponential decay function, and the soil water loss rate was greater in the cropland (0.45-0.70%/day) than that in the treebelt (0.32-0A7%/day). The hydrological relation between treebelt and cropland in the upper soil layer was mainly occurred by treebelt root water uptake from cropland. The biomass of fine treebelt root extended into the cropland decreased logarithmically with the distance from the cropland-treebelt interface, which resulted in the smaller soil water content in the cropland with more proximity to the treebelt. The hydrological relation in the lower soil layer among cropland-treebelt-desert was caused by groundwater recharge, as cropland irrigation raised up the groundwater level to replenish the deep soil layer. The results indicated that the percolation in the cropland was an important water source for the growth of treebelt and desert plants. This study could provide scientific basis for land use pattern design and water resources management in the arid inland river basin. (C) 2014 Elsevier B.V. All rights reserved.
机译:这项研究将干旱内陆河流域的农作物—皮带—荒漠系统作为一个完整的连续体,以研究土壤含水量变化和水文关系。为此,在中国黑河流域绿洲-荒漠过渡带的农田-林木-荒漠-荒漠地带测量了300 cm深度的土壤水分含量和植物根系分布。结果表明,由于频繁的灌溉事件,农田中0-200 cm层的平均土壤水分含量(8.88%)高于林地带(5.78%)和沙漠地区(4.37%)。然而,与树带(18.07%)和沙漠(17.30%)相比,耕地的平均土壤水分明显低于200 cm深度(14.27%),而后者的根系较深以吸收地下水。灌溉事件后农田和林地土壤水分脉动的下降过程可以用指数衰减函数很好地描述,农田中的土壤水分流失率(0.45-0.70%/ day)比林地土壤流失率大。 (0.32-0A7%/天)。上层土壤带与农田的水文关系主要是由于农田吸收带根引起的。进入农田的细林带根的生物量随着距耕地-林带界面的距离呈对数递减,这导致农田中土壤水含量较小,而与林带的距离更大。由于农田灌溉提高了地下水位以补充深层土壤,农田-树木带-荒漠之间较低土壤层的水文关系是由地下水补给引起的。结果表明,农田渗滤是树木带和荒漠植物生长的重要水源。该研究可为干旱内陆河流域土地利用模式设计和水资源管理提供科学依据。 (C)2014 Elsevier B.V.保留所有权利。

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