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From Profile Morphometries to Digital Soil Mapping

机译:从轮廓形式测定到数字土壤映射

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摘要

Soil observation ranges from point observations to spatial evaluation. We can study the clay content at a point or evaluate its distribution across space. Digital morphometries starts with a vision on the soil profile, to extract information from 'inside soils body' and make a diagnostic of its formation history and characters. On the other hand, soil develops as part of the landscape, which presents a continuous vision. Thus, the task is to extrapolate the pedon observation to space, taking us to asoil map, which is the basis for many applications in environmental and agricultural science. This chapter first demonstrates several practical information capture of soil profiles from its visible, near-, and mid-infrared reflectance. This instance tries to answer questions: How can spectroscopy differentiate soil profiles? How can it assist in soil classification? From this, we explore digital soil mapping with several examples. Strategies on soil mapping using pedotechnologies are discussed and exemplified with studies from a simple to complex geology. Finally, we discuss the perspectives of these techniques for getting a full description of soil distribution in the landscape.
机译:土壤观察范围从点观察到空间评估。我们可以在某种程度上研究粘土内容或评估其跨空间的分布。数字形态晶格从土壤轮廓上的视觉开始,从“土壤体内”中提取信息,并诊断其形成历史和人物。另一方面,土壤作为景观的一部分发展,这具有持续的视觉。因此,任务是将PEDON观察推断到空间,使我们带到ASOIL地图,这是环境和农业科学中许多应用的基础。本章首先展示了从其可见,附近和中红外反射率的土壤概况的几种实际信息捕获。这个实例试图回答问题:光谱如何区分土壤配置文件?如何协助土壤分类?由此,我们探索了几个例子的数字土壤映射。使用易于复杂地质学的研究讨论和举例说明了使用PEDOTECHNOLOGIES的土壤映射策略。最后,我们讨论了这些技术的观点,以便在景观中完整描述土壤分布。

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