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Changes in the properties of soils in a solonetz soil complex thirty years after reclamation.

机译:开垦后30年的solonetz土壤复合体中土壤性质的变化。

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The long-term (30 year) dynamics of a solonetz soil complex composed of solonetzic light chestnut soils and chestnut solonetzes under standard conditions and with the application of agromeliorative measures are considered. When the standard zonal agricultural practice is used, the soils of the solonetzic complex have unfavorable agrophysical, chemical, and physicochemical properties and low productivity. After 30 years of the standard three-level tillage of the soils to a depth of 40-45 cm, the productivity of the biogeocenosis decreased. Thirty years after a single rotary-milling subsoil treatment of the 20- to 45-cm soil layer using a milling tool FS-1.3, there were no morphological features pointing to the restoration of the solonetzic process. The humus content in the 0-to 20-cm and 20-to 40-cm soil layers was 2.3 and 1.7%, respectively; the content of adsorbed Na+ in the 20-to 30-cm layer was 11.6% of the total exchange capacity, or 38% lower than its content in the reference soil. The additional yield reached 30-70% and more of that obtained with the standard agricultural technology used during the whole period under investigation. The method of systems biogeotechnology (systems bio-geo engineering) is proposed as a method for the preventive control of soil evolution and the maintenance of the stability and high productivity of the soil cover.Notes Translated from Pochvovedenie (2014) 4, 490-506 (Ru).
机译:考虑在标准条件下并采用农业改良措施时,由松弱的栗色土壤和栗色松树组成的松土壤复合物的长期(30年)动力学。当使用标准的分区农业实践时,松果体复合物的土壤具有不利的农业物理,化学和物理化学特性,且生产力低下。在对土壤进行三层标准耕作30年后,深度达到40-45厘米,生物大面积生产力下降。在使用铣削工具FS-1.3对20至45厘米土壤层进行单次旋转铣削下层土壤处理30年后,没有形态学特征表明恢复了孤石过程。 0至20厘米和20至40厘米土壤层的腐殖质含量分别为2.3和1.7%。 20〜30 cm层中Na + 的吸附量占总交换容量的11.6%,比参考土壤中的含量低38%。在整个调查期间,额外的收成达到了30-70%,并且是使用标准农业技术获得的更多收成。提出了系统生物地理技术方法(系统生物地理工程)作为预防土壤演化和维持土壤覆盖物的稳定性和高生产率的方法。注释摘自Pochvovedenie(2014)4,4,490-506 (Ru)。

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