对腐殖质平衡计算中的侵蚀成分问题进行了探讨

А. Kutova, О. V. Кruglov, V. P. Кoliada
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摘要

本文的目的是介绍在区域领土一级确定水蚀和风蚀对乌克兰波兰区、森林草原区和草原区可耕地土壤腐殖质年损失的影响的结果,这种影响对其平衡产生负面影响。众所周知,在水土流失的影响下,波利西亚地区平均每年不可逆转的土壤流失量为7.6吨/公顷,森林-草原地区为7.8吨/公顷,草原地区为3.3吨/公顷。结果表明,腐殖土流失部分的侵蚀成分接近40%,强化了平衡的负部分。为了获得最准确的土壤腐殖质平衡信息,建议采用差别化方法建立平衡模型。在区域国土水平上,利用本行政区域耕地平均坡度值、特定坡度的土壤冲蚀平均值、土壤和气候条件计算侵蚀导致腐殖质的预测损失。事实证明,计算单个农作物或轮作中腐殖质平衡应包括行政区域内由水侵蚀造成的平均腐殖质损失,乌克兰土壤和气候带各地区之间的差异很大(从154公斤/公顷到1700公斤/公顷)。根据水土流失造成的腐殖质损失总量,确定了3组领土:1 - 50 ~ 100 kg/ha(南草原),2 - 140 ~ 200 kg/ha(波兰、左岸森林草原和北部草原),3 - 200 ~ 300 kg/ha(右岸森林草原)。在有通货膨胀威胁的地区,由风蚀造成的腐殖质损失,在该国南部为293至1700公斤/公顷,严重影响土壤的腐殖质状态,应与水蚀数据一起纳入腐殖质平衡的计算。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
To the issue of the erosion component of calculating the balance of humus
The purpose of the article is to present the results of identifying the influence of water and wind erosion on the annual loss of humus from arable soils of Ukraine in the zones of Polissia, Forest-Steppe and Steppe at the regional territorial level, which negatively affect its balance. It is known that the irreversible annual soil loss under the influence of water erosion on average in the Polissia zone is 7.6, in the Forest-Steppe zone – 7.8, in the Steppe zone – 3.3 t / ha. It is shown that the erosion component in the part of humus losses approaches 40 %, strengthening the negative part of the balance. To obtain the most correct information on the humus balance in soils, a differentiated approach to balance models is recommended. At the regional territorial level, to calculate the predicted losses of humus because of erosion, the value of the average slopes on the arable lands of the administrative region, the average values of soil washout at specific slopes and soil and climatic conditions were used. It is proved that the calculation of the humus balance under individual agricultural crops, or in the crop rotation should include the average, in the administrative region, humus losses caused by water erosion, which differ significantly by regions in the soil and climatic zones of Ukraine (from 154 to 1700 kg/ha). According to the total losses of humus from water erosion, 3 groups of territories were identified: I – from 50 to 100 (South Steppe), II – from 140 to 200 (Polissia, Left-Bank Forest-Steppe and Northern Steppe), III – from 200 to 300 kg/ha (Right-Bank Forest-Steppe). In areas where there is a threat of deflation, the loss of humus caused by wind erosion, which in the southern part of the country ranges from 293 to 1700 kg/ha, significantly affects the humus state of the soil and should be included in the calculations of the humus balance along with the data on water erosion.
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