种植制度对铁砂质热带土壤有机质退化的影响:以塞内加尔南部为例

P. Fernandes, R. Oliver, S. Diatta
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引用次数: 6

摘要

为了评估一种耕作制度的可持续性,了解退化土壤恢复所涉及的机制是必要的。为此,建立了一项为期8年的试验,以测试四种种植制度的效率,这些制度包括施用肥料和/或粪肥,以及作物残留物和/或肥料的掺入,对经过约90年传统种植(花生-谷子轮作,不加任何投入)退化的Haplic Acrisol的再生。测定了处理2年和8年后土壤氮素供给、土壤氮素颗粒大小和化学分布特征,并以此表征土壤有机质(SOM),进而与养分吸收有关。四种试验作物系统中有两种有望恢复土壤肥力(Q1和Q2):4年轮作(包括犁耕休耕、作物残茬和矿物施肥)都对SOM含量有抑制作用,尽管在试验中观察到的总C和总N的损失(例如,第一季度和第二季度分别为-23%和-20% N)比对照(传统种植B, -33% N)要少。只有多年休耕没有导致SOM进一步退化,但没有丰富土壤。另一方面,每年施用10 Mg有机肥干物质(hm -1)与化肥联合施用,显著提高了土壤有机质(仅2年后,全氮增加了2倍),但在8年结束时,这种效果似乎趋于稳定。只有较强的(10 Mg干物质/ 1)和年供给量与矿物施肥相结合,对土壤有机质有积极影响,但其持久性尚未确定。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Changes in Organic Matter of a Ferrallitic Tropical Soil Degraded by Cropping Systems: The Case of Southern Senegal
Understanding of the mechanisms involved in the restoration of degraded soils is necessary in order to assess the sustainability of a cropping system. For this purpose, an 8-year experiment was set up to test the efficiency of four cropping systems involving applications of fertilizer and/or manure and incorporation of crop residues and/or fallows on the regeneration of a Haplic Acrisol degraded by about 90 years of traditional cropping (groundnut-millet rotation without any input). The supply of nitrogen by the soil and particle size and chemical distribution were measured and used to characterize the soil organic matter (SOM) after 2 and 8 years of treatments, and then related to nutrients uptake. Two of the four cropping systems tested that were expected to regenerate soil fertility (Q1 and Q2: 4-year rotations including a plowed-in fallow, incorporation of crop residues, and mineral fertilization) both had a depressive effect on SOM content, although the losses of total C and N observed during the experiment (e.g .,-23% N and -20% N for Q1 and Q2, respectively) were less than that for the control (traditional cropping B, -33% N). Only the multiyear fallow did not result in further degradation of SOM, without, however, enriching the soil. On the other hand, an annual application of 10 Mg dry matter of manure ha -1 , combined with fertilizer, markedly increased the SOM (total N increased by factor 2 after only 2 years), an effect that seemed, however, stabilized at the end of the 8 years. Only a strong (10 Mg dry matter ha -1 ) and annual supply of manure, associated with mineral fertilization, had a positive effect on SOM, but its durability is not established.
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