首页> 外文期刊>Geoderma: An International Journal of Soil Science >Three-dimensional GIS cartography applied to the study of the spatialvariation of soil horizons in a Swiss floodplain
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Three-dimensional GIS cartography applied to the study of the spatialvariation of soil horizons in a Swiss floodplain

机译:三维GIS制图技术在瑞士洪泛区土壤层位空间变化研究中的应用

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In this study, we propose to establish a framework for the study of the spatial variability of the soils found in the floodplain of the Sarine River and for the visualisation of soil distribution patterns in two- and three-dimensions (2-D, 3-D). This environment is characterised by a large lateral and vertical spatial variability of soils that corresponds to the temporal and spatial variations of the fluvial dynamics of the Sarine. The study was carried out using existing Geographical Information System (GIS) functions combined with applications specific to soil cartography. This particular GIS cartography is based on the notion of the soil horizon instead of that of the soil diagnostic profile. A Global Positioning System (GPS) survey was carried out in order to construct a local Digital Elevation Model (DEM) and to ascertain the spatial coordinates for each of the 181 soil obsevation locations. All data were stored in a GIS database, and both landform modeling and soil cartography was undertaken. GIS, ARC/INFO, and Vertical Mapper for MapInfo were adequate for our linear triangulation interpolation, for contour processing and for the creation of cross-sections as well as the corresponding vertical profiles. These vertical profiles served to illustrate the superposition of soil horizons along any line across the sampled area A 3-D representation of soil was obtained using the quadratic finite-element method, which is generally employed in geological studies and which we adapted especially for the representation of soil horizons. 3-D cartography of this type allows the spatial pattern of a given horizon including the variation of its thickness, the superimposition of the different soil horizons, the total soil depth, and the number of horizons at any given location - to be followed through space. Our approach, furthermore, facilitates the perception of soil horizons and their juxtarelationships as 3-D objects, and permits the visualisation of the relationships that exist between any given horizon (or sequence of horizons) and the surface topography. In thus enabling the realistic representation and easy visualisation of the spatial distribution and variability of soils in the landscape, our methodological approach provides a powerful instrument for soil scientists, and a useful decision-support tool for ecosystem management.
机译:在这项研究中,我们建议建立一个框架,用于研究在萨林河河漫滩中发现的土壤的空间变异性,以及可视化二维和三维(2-D,3- D)。这种环境的特征是土壤的横向和垂直空间变化很大,这与盐水井的河流动力学的时空变化相对应。这项研究是利用现有的地理信息系统(GIS)功能以及针对土壤制图的特定应用程序进行的。特定的GIS制图基于土壤层位的概念,而不是土壤诊断轮廓的概念。为了构建本地数字高程模型(DEM)并确定181个土壤观测位置中每个位置的空间坐标,进行了全球定位系统(GPS)调查。所有数据都存储在GIS数据库中,并进行了地形建模和土壤制图。 GIS,ARC / INFO和用于MapInfo的Vertical Mapper足以满足我们的线性三角插值,轮廓处理,横截面创建以及相应的垂直轮廓的需要。这些垂直剖面用于说明沿采样区域的任何直线的土壤层位叠加。使用二次有限元方法获得了土壤的3-D表示法,该方法通常在地质研究中使用,并且我们专门对其进行了调整视野。这种类型的3-D制图可以使给定层位的空间模式包括其厚度的变化,不同土壤层位的叠加,总土壤深度以及任何给定位置处的层位数量在空间中跟随。此外,我们的方法有助于将土壤层位及其并列关系视为3-D对象,并可以可视化任何给定层位(或层位序列)与表面地形之间存在的关系。这样,我们就可以对景观中土壤的空间分布和变异性进行逼真的表示和轻松可视化,我们的方法论方法为土壤科学家提供了强大的工具,并为生态系统管理提供了有用的决策支持工具。

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