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首页> 外文期刊>Ecological indicators >Assessing the relations among the features of the land cover and of the soil on the soil-water interactions through a functional eco-hydrological indicator
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Assessing the relations among the features of the land cover and of the soil on the soil-water interactions through a functional eco-hydrological indicator

机译:通过功能生态水文指标评估土地覆盖特征和土壤土壤的关系

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摘要

Soil Water Repellency (SWR) is an important ecological property that has implications in the soil and water management and is a useful functional eco-hydrological indicator driven by several natural and human factors. In our research we assessed the relationships between SWR and soil properties, broaden the evidence of the influence of land cover on the development of SWR. We also evaluated the relation between SWR and erosion indicators (EI), and we checked the occurrence and severity of distilled water and aqueous ethanol solution repellency before and after the soil samples are compacted (that augmented the soil density in 10%). In the field, we collected superficial soil samples considering the local land cover features, and we assessed the EIs following a pre-established protocol. For evaluating the SWR we used the "drop penetration time" method. Our results show that the soils are mostly neutral (in terms of soil acidity), silt or sandy-textured and chiefly hydrophilic. The texture is an intrinsic soil attribute that primarily influences the relations between soil and water, and the affinity to water is significantly different among the land cover categories. Land cover change induces modifications in the soil surface, and the soil gets more hydrophilic. The EIs helped to evidence such changes caused by land cover changes. Compacted soils led them to be more hydrophilic, regardless of the reagent, being this finding still barely reported in the literature.
机译:土壤防水性(SWR)是一种重要的生态特性,其在土壤和水管理中具有影响,并且是由几种自然和人类因素驱动的有用的功能生态水文指标。在我们的研究中,我们评估了SWR和土壤属性之间的关系,扩大了土地覆盖对SWR发展的影响的证据。我们还评估了SWR和侵蚀指示剂(EI)之间的关系,并且在土壤样品被压实之前和之后检查蒸馏水和乙醇水溶液排斥性的发生和严重程度(增加了10%的土壤密度)。在该领域,我们考虑了浅层土壤样本,考虑到当地土地覆盖功能,我们通过预先成立的协议评估了EIS。用于评估SWR,我们使用了“掉落渗透时间”方法。我们的研究结果表明,土壤大多是中性的(在土壤酸度方面),淤泥或砂质纹理和主要亲水性。纹理是一种内在的土地属性,主要影响土壤和水之间的关系,以及对土地覆盖类别的水性显着不同。陆地覆盖变化会诱导土壤表面的修饰,土壤更加亲水。 EIS帮助证据了土地覆盖变化造成的这种变化。压实的土壤导致它们更亲水,无论试剂如何,这种发现仍然在文献中仍然报道。

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