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首页> 外文期刊>Moscow University Soil Science Bulletin >GENESIS AND GEOGRAPHY OF SOILS HYDROMORPHISM OF CHERNOZEMS IN KAMENNAYA STEP'
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GENESIS AND GEOGRAPHY OF SOILS HYDROMORPHISM OF CHERNOZEMS IN KAMENNAYA STEP'

机译：假面树台阶中蛇纹石的土壤亚型的发生与地理

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摘要

The manifestations of hydromorphic processes and an increase in moisture in chernozems and other steppe soils are related to numerous reasons, both natural and anthropogenic; the following ones should be mentioned: (a) regulation of the hydrological regime of most steppe rivers and streams; hence, they cannot anymore perform their functions of natural drains; (b) disturbance of the land surface and soil runoff by field routes and forest shelter belts; (c) soil compaction by heavy vehicles; (d) recentincrease in atmospheric precipitation in the steppe zone; (e) irrigation without due water control, so that the practically nonpercolative water regime of chernozems shifted to periodically percolative [1]. All this induces the degradation of agroecosystems on chernozems and appearance of hydromorphic plots among the automorphic soils. Consequently, the ground water level went up almost everywhere in the steppe zone, and this rise was the most pronounced in the regions with flat topography, where saucer-like depressions differing in shape and size appeared.
机译：黑钙土和其他草原土壤的水溶过程和水分增加的表现与自然和人为的多种原因有关。应提及以下内容：（a）调节大多数草原河流和溪流的水文状况;因此，他们不再能够发挥自然排水系统的功能; （b）野外路线和森林防护带对土地表面和土壤径流的干扰; （c）重型车辆压实土壤; （d）草原地区近期大气降水增加; （e）在没有适当的水控制的情况下进行灌溉，以使黑钙土的实际上非渗透性的水态转换为周期性渗透[1]。所有这些都会导致黑钙土上的农业生态系统退化，并导致自养土壤中出现水培图。因此，在草原区几乎所有地方的地下水位都在上升，这种上升在地形平坦的地区最为明显，那里出现了形状和大小不同的碟状凹陷。

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