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首页> 外文期刊>Geoderma: An International Journal of Soil Science >Soil hydrological and erosional responses in patches and inter-patches in vegetation states in semi-arid Australia.
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Soil hydrological and erosional responses in patches and inter-patches in vegetation states in semi-arid Australia.

机译:半干旱澳大利亚植被状态下斑块和斑块之间的土壤水文和侵蚀响应。

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摘要

Resource retention is an important component of landscape function in semi-arid environments, with patches in the landscape serving as sink zones, capturing runoff, sediments and nutrients from inter-patches or source areas. The overall aim of this study was to compare the hydrological and erosional responses of patches and inter-patches using small-scale (1 m2) rainfall simulation in four vegetation states comprising woody encroachment (trees and shrubs >1200 stems ha-1), recent pasture (<23 years of age), long-established pasture (50-100 years of age) and open woodland in relation to ground cover, in semi-arid south-eastern Australia. Hydrological and erosional responses differed consistently between patches and inter-patches within each vegetation state. Inter-patches (mean ground cover=23.5%+or-2.7% SE) had the least desirable hydrological and erosional responses, and produced the highest amounts of runoff and sediment, followed in decreasing order by medium vegetated patches (mean ground cover=54.8%+or-3.1% SE) and well vegetated patches (mean ground cover=77.3%+or-3.1% SE). However, when hydrological and erosional responses from the same patch type and inter-patches were compared between vegetation states, two differences were found. Well vegetated patches in woody encroachment produced higher runoff than other well vegetated patches, and inter-patches in recent pasture had higher sediment concentration and production than inter-patches in other vegetation states. Total ground cover in the patch types was negatively correlated with runoff and sediment production, and with sediment production in inter-patches. Cryptogam cover in well vegetated patches was associated with higher runoff and sediment production, but cryptogam cover in inter-patches was associated with lower sediment concentration and production. Herbaceous cover and litter in medium vegetated patches were associated with lower runoff and sediment production. Our results indicate that patches and inter-patches are functional units from an eco-hydrological perspective within this semi-arid region and they influence soil hydrological and erosional characteristics irrespective of vegetation state.Digital Object Identifier http://dx.doi.org/10.1016/j.geoderma.2010.10.024
机译:资源保留是半干旱环境中景观功能的重要组成部分,景观中的斑块用作汇区,捕获斑块间或源区的径流,沉积物和养分。这项研究的总体目的是使用小规模(1 m 2 )降雨模拟比较包括木本侵蚀(树木和灌木>在内)的四种植被状态下的斑块和斑块之间的水文和侵蚀响应在半干旱的南部地区,有1200茎ha -1 ),最近的牧场(<23岁),历史悠久的牧场(50-100岁)和与地被植物相关的开阔林地-澳大利亚东部。在每个植被状态下,斑块之间和斑块之间的水文和侵蚀响应始终是不同的。斑块间(平均地面覆盖率= 23.5%+或-2.7%SE)具有最不理想的水文和侵蚀响应,并产生最大量的径流和沉积物,其次是中度植被覆盖的补丁(平均地面覆盖率= 54.8 %+或-3.1%SE)和植被良好的补丁(平均地面覆盖率= 77.3%+或-3.1%SE)。但是,在比较植被状态之间相同补丁类型和补丁之间的水文和侵蚀响应时,发现了两个差异。木本性植被中植被良好的斑块比其他植被良好的斑块产生更高的径流,并且最近牧场的斑块间的沉积物浓度和产量高于其他植被状态的斑块间。斑块类型中的总地面覆盖与径流和泥沙产生以及各斑块之间的泥沙产生呈负相关。植被良好的斑块中的隐孢子虫覆盖物与较高的​​径流和沉积物产生有关​​,而斑块间的隐性隐孢子虫的覆盖物与较低的沉积物浓度和产生物相关。中度植被覆盖区的草本覆盖物和凋落物与较低的径流和沉积物产生有关​​。我们的结果表明,从生态水文学的角度来看,该斑块和斑块之间是该半干旱地区的功能单位,并且无论植被状态如何,它们都会影响土壤水文和侵蚀特征。数字对象标识符http://dx.doi.org/ 10.1016 / j.geoderma.2010.10.024

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