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首页> 外文期刊>Vadose Zone Journal >Eco-Geophysical Imaging of Watershed-Scale Soil Patterns Links with Plant Community Spatial Patterns
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Eco-Geophysical Imaging of Watershed-Scale Soil Patterns Links with Plant Community Spatial Patterns

机译:流域尺度土壤格局与植物群落空间格局的生态地球物理成像

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Received for publication 19 June 2008. The extent to which soil moisture and nutrient availability control the structure, function, and diversity of plant communities has aroused considerable interest in the past decade and remains topical in light of global change. Numerous plant communities are controlled either by water or soil nutrient availability, and yet spatial patterns of soil properties affecting resource pools, such as texture, are often poorly delineated at the landscape level. Traditional soil survey methods, developed for land evaluation, remain largely qualitative, based on the subjective analysis of the soil surveyor and often using vegetation patterns to demarcate soil boundaries. To date, no independent method of determining the properties of soil root-zone spatial patterns has been developed for use at the landscape scale, resulting in a knowledge gap between observed aboveground vegetation patterns and the distribution of belowground soil properties. The objective of this work was to determine whether a quantitative link could be observed between bulk soil electrical conductivity, used as an indicator of soil texture, and the plant community spatial pattern using geophysics. By comparing the geophysical signal with plant community patterns, we have discovered distinct vegetation niches corresponding to distinct zones of bulk soil electrical conductivity. A hierarchical ranking of the mean bulk soil electrical conductivity for each plant community type follows a power-law structure.
机译:于2008年6月19日公开发表。在过去的十年中,土壤水分和养分的可利用性在多大程度上控制了植物群落的结构,功能和多样性,引起了人们的极大兴趣,并且鉴于全球变化,这仍然是热门话题。许多植物群落都受到水或土壤养分可用性的控制,但是影响资源库的土壤属性的空间模式(例如质地)在景观水平上通常很难被描绘出来。为评估土地而开发的传统土壤调查方法在很大程度上仍具有定性,这是基于对土壤调查员的主观分析,并且经常使用植被模式来划分土壤边界。迄今为止,尚未开发出确定土壤根区空间格局特性的独立方法以用于景观尺度,从而导致观测到的地上植被格局与地下土壤特性分布之间存在知识鸿沟。这项工作的目的是确定是否可以在作为土壤质地指标的散装土壤电导率与使用地球物理学的植物群落空间格局之间建立定量联系。通过将地球物理信号与植物群落模式进行比较,我们发现了与散装土壤电导率不同区域相对应的独特植被生态位。每个植物群落类型的平均土壤电导率的等级排序遵循幂律结构。

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