俄罗斯新数字土壤地图上的北极和苔原土壤,比例尺1:2.5米

Q4 Agricultural and Biological Sciences Biulleten'' Pochvennogo instituta im VV Dokuchaeva Pub Date : 2020-03-27 DOI:10.19047/0136-1694-2020-101-46-75
T. Ananko, M. Gerasimova, D. Konyushkov
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引用次数: 6

摘要

V.V.Dokuchaev土壤科学研究所发起了一个项目,在俄罗斯联邦土壤图1:2.5 M比例尺(1988年)的基础上,编制一份新的俄罗斯数字土壤图,该地图在意识形态和命名上对俄罗斯土壤实质性遗传分类系统(CSRS)进行了修订和解释。第一阶段意味着将原始地图上的土壤制图单位转换为CSRS,并将属性数据库中的土壤相应重命名为每个土壤多边形的地图数字化版本。在第二阶段,利用数字土壤测绘技术、基础土壤图和新材料,包括卫星图像和数字高程模型,开发了一个新的土壤覆盖数字模型。图例部分“苔原土壤”包含16个土壤单元,形成自己的区域或在各种组合(土壤复合体)中发现。由于对每个土壤多边形进行了重新分类和仔细分析,北极和亚北极苔原的土壤在新地图上获得了更详细、更具差异性的表示,Блле。В。2020年Вып。101.Dokuchaev土壤公报,2020,101 48已经规定了基于剖面形态和主要土壤特性的诊断。地图初始内容的最显著变化涉及SMRF上被称为潜育土的土壤。已经指定了一组单独的冻土。弱发育土壤(岩土、砂土和pelozems)和岩土首次出现在地图上。建议对具有分类和非分类圆圈的“斑点苔原”土壤和具有低温裂缝和裂缝的土壤进行差异决策。这项研究的结果使改进CSRS中土壤的诊断和命名成为可能。
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Arctic and tundra soils on the new digital soil map of Russia, 1 : 2.5 M scale
V.V. Dokuchaev Soil Science Institute has initiated a project on compilation of a new Digital Soil Map of Russia on the basis of the Soil Map of the Russian Federation (SMRF) 1 : 2.5 M scale (1988) revised and interpreted in ideology and nomenclature of the new substantive-genetic Classification System of Russian Soils (CSRS). The first stage implies the conversion of soil mapping units on the original map into the CSRS with a corresponding renaming of soils in the attribute database to the digitized version of the map for each soil polygon. During the second stage, a new digital model of the soil cover is developed with the use of digital soil mapping technologies, basic soil map, and new materials, including satellite images and digital elevation models. The legend section “Tundra Soils” contains 16 soil units forming their own areas or found in various combinations (soil complexes). As a result of the reclassification and careful analysis of each soil polygon, the soils of Arctic and Subarctic tundra have obtained a more detailed and differential representation on the new map, and Бюллетень Почвенного института им. В.В. Докучаева. 2020. Вып. 101. Dokuchaev Soil Bulletin, 2020, 101 48 their diagnostics based on the morphology of the profiles and major soil properties have been specified. The most significant changes in the initial content of the map concern the soils referred to as gley soils on the SMRF. A separate group of cryozemic soils has been specified. Weakly developed soils (petrozems, psammozems, and pelozems) and lithozems have been introduced on the map for the first time. Differential decisions are suggested for the soils of “spotty tundra” with sorted and nonsorted circles and for the soils of cryogenic fissures and cracks. The results of the study have made it possible to refine the diagnostics and nomenclature of soils in the CSRS.
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发文量
15
审稿时长
8 weeks
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