Agrogenic changes in the properties of dark chestnut virgin and arable soil with different use and irrigation

L. Vorotyntseva, V.I. Nikoliuk
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Abstract

In the article, it was provided a comparative analysis of the ecosystem significance of soil characteristics transformed as a result of changes in the use conditions. At the three monitoring stationary sites in the Chaplinka district of the Kherson region, we studied the properties of dark chestnut soil (Haplic Kastanozem) on virgin lands (a biosphere reserve "Askania-Nova") and with more than a hundred years of use in agricultural production without irrigation and with a 50-year irrigation with water from the Kakhovsky trunk canal. Changes in the salt regime of the soil and the composition of exchangeable cations were established. In irrigation the total content of water-soluble salts up to 0.14-0.21% (toxic salts ‒ up to 0.06-0.15 %) was increased. The composition of salts was changed, their migration and accumulation in the lower soil layers. Under the influence of fresh water irrigation the process of dealkalinization in the dark chestnut soil took place. The involvement of virgin soil in agricultural use led to a decrease in the total content of humus and the transformation of its group composition. The content of humic acids (HA) was decreased. The content of fulvic acids (FA) was increased. The HA/FA ratio in the 0-10 cm layer changed from 2.6 (in virgin soil) to 1.6 in irrigated soil. The plowing and agricultural use of the dark chestnut soil led to a change in the state of the microbial cenosis. The number of microorganisms assimilating mineral and organic nitrogen, actinomycetes, oligotrophs, and eutrophs were increased. With irrigation the degree of transformation of the microbial cenosis increases. The indicator of biological degradation of irrigated dark chestnut soil was 4 %. This corresponds to a low level of degradation. A set of 10 indicators of the quality of the studied soil was proposed for calculating the level of its provision of ecosystem services (supplying and supporting). The algorithm and calculation results are presented. The soil of all monitoring sites of Markeev station is characterized by a high level of provision of ecosystem services. In virgin soil it was 8.3 points; in arable soil without irrigation it was 7.2, and with irrigation it was 7.5 points.
不同利用方式和灌溉方式对黑栗子原生土和耕地土壤性状的影响
对比分析了利用条件变化对土壤特征变化的生态系统意义。在Kherson地区Chaplinka区的三个监测固定站点,我们研究了未开垦土地(一个生物圈保护区“Askania-Nova”)上的黑栗子土(Haplic Kastanozem)的特性,这些土壤在农业生产中使用了100多年而没有灌溉,并且使用了50年的卡霍夫斯基干渠的水灌溉。确定了土壤盐态和交换阳离子组成的变化。灌溉水溶盐总含量提高了0.14 ~ 0.21%(有毒盐0.06 ~ 0.15%)。盐类的组成发生了变化,并在下层土壤中迁移和积累。在淡水灌溉的影响下,黑栗子土发生了脱碱化过程。未开垦土壤参与农业利用导致腐殖质总含量降低,类群组成发生变化。腐植酸(HA)含量降低。黄腐酸(FA)含量增加。灌溉土0 ~ 10 cm土层的HA/FA比值由原生土的2.6变化为1.6。黑栗子土的耕作和农业利用导致了微生物群落状态的变化。吸收无机氮和有机氮的微生物、放线菌、寡养菌和富营养菌的数量增加。随着灌溉的增加,微生物群落的转化程度增加。灌溉黑板栗土的生物降解指标为4%。这对应于低水平的退化。提出了一套10个土壤质量指标,用于计算土壤提供生态系统服务(供应和支持)的水平。给出了算法和计算结果。Markeev监测站各监测点土壤具有较高的生态系统服务水平。在未开垦的土地上,它是8.3分;在未灌溉的耕地中,得分为7.2分,有灌溉的耕地中得分为7.5分。
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