Characteristics of humus content on different soil types of Zdolbuniv district of Rivne Region

N. Dmitrievtseva, O. Veremchuk, S. Pilipaka, O. Hryshchenko
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Abstract

The dynamics of changes in the humus state of the soils of Zdolbuniv district during the V–XI rounds of agrochemical survey were analyzed. The state of biologization of agriculture, in particular the plowing of siderates, the introduction of straw and manure and the use of peat over the last 8 years in the studied area, is highlighted. Mandatory biologization of agriculture, taking into account the biological features of each crop, in particular, plant needs for nutrients, indicators of potential and effective soil fertility, its physical and chemical properties, assortment and chemistry of fertilizers, climatic conditions in a zonal section — comprehensive implementation of these measures will contribute to a significant increase soil fertility of the district’s agricultural lands, in particular improving its humus condition. Since an important reason for the lack of accumulation of humus reserves in the studied soils is the unsatisfactory state of biologicalization of agriculture in the area. Conclusions and suggestions on improving the humus condition of the soils of the studied area have been prepared. It is established that according to the results of agrochemical studies of agricultural lands of Zdolbuniv district of Rivne region for the XI round of agrochemical certification of agricultural lands, the weighted average humus content is 2.6% and corresponds to the average content. It was found that the studied soils of the district are characterized by very low and low (less than 2.1%) — 0.86 thousand hectares (10.0%), medium (from 2.1 to 3.0%) — 6.14 thousand hectare (71.7%), elevated (from 3.1 to 4.0%) — 1.5 thousand hectare (17.5%), high and very high (> 4%) — 0.06 thousand hectare (0.7%) humus content. In terms of the main types of soils, the highest humus content in meadow soils, meadow and chernozem soils, chernozem and meadow soils with content of 3.3% and on chernozems typical and chernozems strongly degraded of different degrees of erosion with an average humus content of 2.8%. It should be noted that the dynamics of humus content in the soils of Zdolbuniv district of Rivne region for the last 10 years of research shows the process of its stabilization and increase from 2.2% in 2007 to 2.6% in 2017. Comparing only the area of land plots, which were surveyed in three rounds — 2007, 2012 and 2017, the humus content is 2.5; 2.5 and 2.6%, respectively, which confirms the stabilization of the humus content over the past ten years of agrochemical research. An important reason for the lack of accumulation of humus reserves in the studied soils is the unsatisfactory state of biologization of agriculture in the area.
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河区Zdolbuniv地区不同土壤类型腐殖质含量特征
分析了第v - 11轮农化调查期间Zdolbuniv地区土壤腐殖质状态的变化动态。重点介绍了该研究地区过去8年来的农业生物化状况,特别是siderate的耕作、秸秆和粪肥的引进以及泥炭的使用。强制性农业生物化,考虑到每一种作物的生物特性,特别是植物对养分的需求、潜在和有效土壤肥力指标、其物理和化学特性、肥料的分类和化学、地带性剖面的气候条件这些措施的全面实施将有助于显著提高该地区农业用地的土壤肥力,特别是改善其腐殖质状况。由于研究土壤中腐殖质储量缺乏积累的一个重要原因是该地区农业生物化状况不理想。提出了改善研究区土壤腐殖质状况的结论和建议。根据里夫纳大区Zdolbuniv区农用地第11轮农化认证农用地农化研究结果确定,腐殖质加权平均含量为2.6%,与平均含量相对应。研究区土壤腐殖质含量表现为极低和极低(低于2.1%)~ 0.86万公顷(10.0%)、中等(2.1 ~ 3.0%)~ 6.14万公顷(71.7%)、高(3.1 ~ 4.0%)~ 1.5万公顷(17.5%)、高和极高(> 4%)~ 0.06万公顷(0.7%)。从主要土壤类型来看,草甸土、草甸黑钙土、黑钙土和草甸土腐殖质含量最高,为3.3%,典型黑钙土和不同侵蚀程度强烈退化的黑钙土平均腐殖质含量为2.8%。值得注意的是,在过去10年的研究中,里夫纳地区zdolbuuniv地区土壤中腐殖质含量的动态变化表明,其稳定并从2007年的2.2%增加到2017年的2.6%。仅比较2007年、2012年和2017年三轮调查的地块面积,腐殖质含量为2.5;分别为2.5%和2.6%,这证实了过去十年农化研究中腐殖质含量的稳定。研究土壤中腐殖质储量缺乏积累的一个重要原因是该地区农业生物化状况不理想。
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