首页> 外文期刊>Eurasian Soil Science >Changes in the salinity of solonetzic soil complexes of the Ergeni Upland under long-term anthropogenic impact (soil studies at the Arshan'-Zel'men Experimental Station of the Russian Academy of Sciences)
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Changes in the salinity of solonetzic soil complexes of the Ergeni Upland under long-term anthropogenic impact (soil studies at the Arshan'-Zel'men Experimental Station of the Russian Academy of Sciences)

机译:长期人为影响下额尔古尼山地松材化土壤复合物的盐度变化(俄罗斯科学院Arshan'-Zel'men实验站的土壤研究)

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摘要

Unique experiments performed since the 1950s at the Arshan'-Zel'men Experimental Station have formed the basis for afforestation in the dry steppe and semidesert zone without irrigation on the salt-affected soils of solonetzic soil complexes of the Ergeni Upland. Ameliorative measures favored the accumulation of productive moisture in the upper 2-m-thick soil layer, which ensured the growth of trees and the partial leaching of soluble salts to a depth of 1-1.4 m. However, no complete desalinization of the soil profiles took place. The degree of removal of exchangeable sodium from the exchange complex (soil dealkalization) was smaller. The monitoring of changes in the salt status of the soils upon agroforest reclamation was performed until the early 1980s. Our investigations of 2005-2006 showed that the soil amelioration is still in progress: the salt maximum in the profile of the solonetzes descended to a depth of 2.2 m, and the exchangeable sodium was lost from the plow layer (0-40 cm). Plowed soils between forest shelterbelts were also subjected to desalinization and dealkalization of their soil profile, though less intensely than those under the shelterbelts.
机译:自1950年代以来在Arshan'-Zel'men实验站进行的独特实验,为在Ergeni高原的盐碱土复合体上无盐灌溉的干旱草原和半干旱地区造林奠定了基础。改善措施有利于生产性水分在厚度为2米的上部土壤层中的积累,从而确保树木的生长和可溶性盐的部分浸出至1-1.4 m的深度。但是,土壤剖面没有完全脱盐。从交换复合物中除去可交换钠的程度(土壤脱碱)较小。直到1980年代初,对农林复垦后土壤盐分状况的监测一直在进行。我们在2005年至2006年的调查表明,土壤改良仍在进行中:孤石剖面中的盐分最大值下降至2.2 m的深度,可耕层(0-40 cm)损失了可交换的钠。森林防护林带之间的耕作土壤也经历了土壤剖面的脱盐和脱碱处理,尽管强度不如防护林带之下的土壤强。

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