利用数字高程模型对斜坡土壤进行详细制图

IF 0.3 Q4 GEOLOGY
Alla Oleksandrivna Achasova, А. О. Ачасова, А. О. Сєдов
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引用次数: 1

摘要

问题的表述。乌克兰目前的农业发展阶段需要高度翔实的土壤地图。创建此类地图的方向之一是使用数字高程模型(DEM)作为土壤特征的空间转换器。文献综述表明,尽管有大量关于这一主题的出版物,土壤数字制图的一些问题仍然相关。本文的目的是研究在创建详细的数字地面地图时使用地形指示模型的可能性。这项研究是在试验场境内进行的。在填埋场的实地研究中,确定了土壤以黑钙土为代表,具有不同侵蚀程度的典型特征。建议使用旱胚性系数来定量描述地形对土壤形成的影响,表征与水平表面相比,特定地形部分的热液条件的变化。使用“幻影3”无人机获得了详细的DTM。在此基础上建立了多个地形参数的导数模型。建立了该地区旱胚性的数字模型,并将其转换为有机碳(C)含量模型。指定的地图显示了土壤覆盖的初始条件。它可以作为比较现代土壤参数的标准,以评估其退化程度。与实际碳含量图的比较表明,由于人为退化,研究区土壤碳的平均损失可估计为每吨土壤5.1千克。调查证明,地貌的地理信息分析可以定量地确定某一地区土壤形成的热液条件。基于这种方法构建的制图材料表征了土壤地层的景观潜力,反映了土壤的准处女地状况。具有科学新颖性和现实意义。详细的土壤图,基于实地和实验室土壤研究的结果,导致了文章中潜在的DEM分析土壤评估,允许充分估计和客观地表示坡地侵蚀和旱性土壤及其复体的分布。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
The use of digital elevation models for detailed mapping of slope soils
Formulation of the problem. The current stage of agricultural development in Ukraine requires highly informative soil maps. One of the directions for creating such maps is the use of digital elevation models (DEM) as a spatial translator of soil characteristics. The literary review has showed that despite the large volume of publications on this topic, a number of issues of soils digital mapping remain relevant. The purpose of the article is to study the possibilities of using relief-ground indicative models in creation of detailed digital ground maps. Methods. The research was conducted on the territory of the testing ground. During the field study of the landfill, it has been established that the soils are represented by chernozem typical of varying erosion degrees. It is proposed to use a xeromorphism coefficient for the quantitative account of the landforms influence on soil formation, characterizing changes in hydrothermal conditions for a particular section of the topography, compared with the horizontal surface. A detailed DTM was obtained, using the "Phantom 3" UAV.The derivative models of a number of topographic parameters were built on its basis later. A digital model of xeromorphism of the territory was built, transformed into a model of organic carbon (C) content. The specified map shows initial conditions of the soil cover. It can be used as a standard to compare parameters of modern soils for assessment of extent of their degradation. Comparison of this map with the map of actual C content has shown that average loss of C by soils of the studied area owing to anthropogenic degradation can be estimated at 5.1 kg on 1 t of the soil. Results. Investigations have proved that the geoinformation analysis of landforms allows to quantitatively shape hydrothermal conditions of soil formation for a certain territory. The cartographic materials constructed on such a methodical approach characterize landscape potential on soil formations and reflect quasi-virgin land condition of the soil. Scientific novelty and practical significance. The detailed soil maps, based on the results of field and laboratory soil studies, leading to potential soil assessment for DEM analysis in the article, allow to adequately estimate and objectively represent distribution of eroded and xeromorphic soils and their complexes on sloping lands.
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