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Ecohydrological adaptation of soils following land abandonment in a semi-arid environment

机译:半干旱环境下土地遗弃后土壤的生态水文适应

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Representative land use types were selected in southeast Spain to investigate the redistribution of soil water in relation to vegetation development and land abandonment. Simulated rainfall experiments were performed during 2 days on each of the four selected surfaces: ploughed, a 3-year fallow field, a 12-year abandoned field with shrubs and a semi-natural field with Stipa tenacissima tussocks. Each experiment consisted of five runs of artificial rain. Soil moisture dynamics were measured by time domain reflectometry (TDR), as well as runoff and ponding on the plot surface. Also the movement of the wetting front was measured after each run. On the ploughed field, ponding and local runoff were less important with shallow and homogeneous wetting fronts. The other land uses showed increased heterogeneity in wetting front development, with soil water pockets under the plants that moved down at greater velocities than under the bare inter-spaces. It is hypothesized that S. tenacissima and possibly Artemisia herba-alba adapt their environment by capturing water through stem-root flow systems to divert water to deeper soil layers to reduce evaporation. Furthermore it is suggested that during vegetation development soil heterogeneity increases, as expressed by the water infiltration patterns observed, and that the bare inter-patches are important in the infiltration process.
机译:在西班牙东南部选择了代表性的土地利用类型,以调查土壤水与植被发展和土地放弃有关的再分配。在两个选定的表面中的每一个上,在2天之内进行了模拟降雨实验:耕作,3年休耕地,12年废弃灌木地和半天然田间针茅草。每个实验由五次人工降雨组成。通过时域反射仪(TDR)以及样地表面的径流和积水来测量土壤水分动力学。在每次运行后,还测量了润湿前沿的运动。在耕地上,浅层和均质的湿润锋面对池塘和局部径流的影响较小。其他土地利用表现出在湿润前沿发育中的非均质性增加,植物下方的土壤水袋以比裸露的空隙下更大的速度向下移动。据推测,S。tenacissima和可能的Artemisia herba-alba通过茎根流系统捕获水以将水转移到更深的土壤层以减少蒸发,从而适应了环境。此外,有人建议,在植被发育过程中,土壤异质性会增加,如观察到的水渗透模式所表明,裸露的斑块在渗透过程中很重要。

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