不同耕作和施肥制度下典型黑钙土和异腐土的理化和农化指标

Y. Kravchenko, Olha Bykova
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摘要

检查土壤的理化和农化指标的相关性在于,这些特性决定了农作物的产量和质量,从而影响到整个国家的粮食安全。在这方面,研究的目的是建立不同土壤耕作和施肥技术对典型黑钙土和等腐殖质土壤理化和农化指标剖面分布的长期影响。常规耕作条件下,典型黑钙土表层养分分布均匀,10 ~ 40 cm土层养分含量最高。在水土保持耕作条件下,典型黑钙土0 ~ 20 cm土壤有效水解氮、流动磷和交换钾含量最高,分别为192.30±22.44和192.51±22 mg/kg;63.57±5.762和62.07±0.312 mg/kg;浅埋(RTu)和深埋(DRTu)土壤保持耕作分别为527.14±36.204和465.27±5.844 mg/kg。在典型黑钙土0 ~ 100 cm土层中,DRTu处理下植物养分含量最高,CTu次之。在中国异葎草中,免耕土壤0 ~ 10 cm范围内NH4 + -N和NO3 -N的积累量较高,而在20 ~ 40 cm范围内,翻耕导致这些养分的积累量较大。全磷含量随深度变化不显著。典型黑钙土在施用化肥的条件下,各耕作处理的养分含量和培养基的反应值均有所增加。交换性钙和镁的含量在施肥投入品上变化不大。本研究结果表明,在限制肥料利用的条件下,利用作物残茬氮补偿和覆盖作物与矿物肥料配合使用,可以维持黑钙土的肥力水平
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Physico-chemical and agrochemical indicators of typical chernozem and isohumisol under various tillage and fertiliser systems
The relevance of examining the physico-chemical and agrochemical indicators of soils lies in the fact that these properties determine the level and quality of agricultural crops, thus affecting the food security of the country as a whole. In this regard, the purpose of the study is to establish the longterm impact of different soil tillage and fertilisation technologies on the profile distribution of physicochemical and agrochemical indicators of typical chernozem and isohumisol soils. Under conventional tillage (CTu), plant nutrients were evenly distributed within the upper layer of typical chernozem, with the highest values observed in the 10-40 cm depth range. Under soil conservation tillage, with the addition of straw at a rate of 1.2 t/ha+N12+N78P68K68, the content of available hydrolyzable nitrogen, mobile phosphorus, and exchangeable potassium in the typical chernozem soil was highest in the 0-20 cm layer: 192.30±22.44 and 192.51±22 mg/kg; 63.57±5.762 and 62.07±0.312 mg/kg; 527.14±36.204 and 465.27±5.844 mg/kg for shallow (RTu) and deep (DRTu) soil conservation tillage, respectively. In total at 0-100 cm layer of typical chernozem, the highest content of plant nutrients was observed under DRTu followed by CTu. In Chinese isohumisol, a higher accumulation of NH4 + -N and NO3 -N was observed in the 0-10 cm depth range under no-till soil management, while in the 20-40 cm depth range, plowing resulted in greater accumulation of these nutrients. The total phosphorus content did not notably change with depth. Under the application of fertilisers, the content of nutrients and the reaction value of the medium increased for all tillage treatments of typical chernozem. The content of exchangeable calcium and magnesium did not change considerably on the fertilised inputs. The findings of this study indicate the feasibility of using crop residues with nitrogen compensation and cover crops, in conjunction with mineral fertilizers, to maintain the fertility level of chernozem soils under conditions of limited manure utilisation
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