Soil cover structure and transformation of morphometric parameters of Haplic Chernozems under no-tillage

Q4 Agricultural and Biological Sciences
V. Belobrov, S. Yudin, N. Ermolaev, A. Y. Aidiev
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Abstract

The results of the field experiment have been analyzed, it was set up on two experimental fields (with an area of 2.4 hectares each), where two different agricultural techniques – traditional and no-till – were applied. Diagnostics of morphometric parameters of typical chernozems such as: the thickness of the A1 horizon, A1 + AB horizons and the depth of carbonates reaction with 10% HCl, has shown that some changes in soils and soil cover had occurred in the fields over 8 years. The integral indicator of soil productivity is the thickness of the humus horizon, it demonstrated trends to decrease and increase in the soil cover structure of the experimental fields with different compositions of chernozem subtypes. The trends result from both climate change and periodic dry periods, which are not typical of the region, and from the change of traditional technology to no-till. The carbonates leaching from chernozem profiles in all variants of the experiment decreased, which correlates well with climatic indicators, changing with the seasons of the year. Chernozems with thin humus layaer and reacting with HCl close to the surface do not require liming. The revealed changes are not statistically significant, they reflect the resistance of chernozems to the variability of natural and anthropogenic factors of soil formation. Crop residues on the soil surface under no-tillage reduce physical evaporation, which contributes to moisture accumulation in the soil. The use of cover crops in winter also increases the moisture reserves, which are consumed by the plants during the summer growing season. Information on the transformation of morphometric parameters allows making temporal and spatial corrections in the applied agricultural practices (crop rotation, fertilization, the use of cover crops, herbicides and pesticides).
免耕条件下单立地黑钙土覆盖结构及形态计量参数的变化
对田间试验的结果进行了分析,在两个试验田(每个试验田面积为2.4公顷)上进行了两种不同的农业技术——传统和免耕。对典型黑钙土A1层厚度、A1 + AB层厚度、碳酸盐与10% HCl反应深度等形态计量参数的诊断表明,8年来大田土壤和土壤覆盖发生了一定的变化。土壤生产力的综合指标是腐殖质层厚,不同黑钙土类型组成的试验田土壤覆盖结构呈现出减少和增加的趋势。这种趋势是由于气候变化和周期性干旱期(这在该地区并不典型)以及传统技术向免耕的转变造成的。黑钙土剖面碳酸盐浸出量在各试验变量中均呈下降趋势,与气候指标有较好的相关性,且随季节变化。腐殖质层薄且靠近地表与盐酸反应的黑钙土不需要施石灰。这些变化在统计学上不显著,反映了黑钙土对土壤形成的自然和人为因素的变异性的抵抗力。免耕条件下,作物残留在土壤表面减少了物理蒸发,有利于土壤水分积累。在冬季使用覆盖作物也增加了水分储备,这些水分在夏季生长季节被植物消耗。关于形态计量参数转换的信息可以对应用的农业做法(作物轮作、施肥、覆盖作物的使用、除草剂和杀虫剂)进行时空校正。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
CiteScore
0.90
自引率
0.00%
发文量
15
审稿时长
8 weeks
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