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Significant build-up of soil organic carbon under climate-smart conservation farming in Sub-Saharan Acrisols

机译:撒哈拉沙漠以南地区的气候聪明保护性耕作下土壤有机碳的大量积累

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Conservation farming (CF) involving minimumtillage, mulching and crop rotation may offer climate change adaptation and mitigation benefits. However, reported effects of CF, as applied by smallholders, on storage of soil organic carbon (SOC) and soil fertility in Sub-Saharan Africa differ considerably between studies. This is partly due to differences in management practice, soil type and adoption level between individual farmers. Where CF involves planting basins, year-to-year changes in position of basins make SOC stock estimates more uncertain. Here we assess the difference in SOC build-up and soil quality between inside planting basins (receiving inputs of lime and fertilizer; basins opened each year) and outside planting basins (no soil disturbance or inputs other than residues) under hand-hoe tilled CF in an Acrisol at Mkushi, Zambia. Seven years of strict CF husbandry significantly improved soil quality inside planting basins as compared with outside basins. Significant effects were found for SOC concentration (0.74 +/- 0.06% vs. 0.57 +/- 0.08%), SOC stock (20.1 +/- 2.0 vs. 16.4 +/- 2.6 t ha(-1), 0-20 cm), soil pH (6.3 +/- 0.2 vs. 4.95 +/- 0.4) and cation exchange capacity (3.8 +/- 0.7 vs. 1.6 +/- 0.4 cmol(c) kg(-1)). As planting basins only occupy 9.3% of the field, the absolute rate of increase in SOC, compared with outside basins, was 0.05 t C ha(-1) yr(-1). This corresponds to an overall relative increase of 2.95% SOC yr(-1) in the upper 20 cm of the soil. Also, hot water extractable carbon (HWEC), a proxy for labile organic matter, and potential nitrification rates were consistently greater inside than outside basins. The significant increase in quantity and quality of SOC may be due to increased inputs of roots, due to favorable conditions for plant growth through input of fertilizer and lime, along with increased rainwater infiltration in the basins. (c) 2019 Elsevier B.V. All rights reserved.
机译:涉及最小耕作,覆盖和轮作的保护性耕作(CF)可以提供适应和缓解气候变化的好处。但是,在小规模研究中,据报道小农使用的CF对撒哈拉以南非洲土壤有机碳(SOC)的存储和土壤肥力的影响差异很大。部分原因是各个农民之间在管理实践,土壤类型和收养水平上存在差异。在CF涉及种植盆地的情况下,盆地位置的逐年变化使SOC存量估算更加不确定。在这里,我们评估了用手hoe耕作的CF下种植盆内部(接收石灰和肥料输入;每年开放的盆)与外面种植盆(没有土壤干扰或除残留物以外的输入)之间SOC累积和土壤质量的差异。在赞比亚Mkushi的Acrisol中。与外部流域相比,七年严格的CF饲养显着改善了种植流域内部的土壤质量。发现SOC浓度(0.74 +/- 0.06%vs.0.57 +/- 0.08%),SOC储备(20.1 +/- 2.0 vs. 16.4 +/- 2.6 t ha(-1),0-20 cm ),土壤pH(6.3 +/- 0.2对4.95 +/- 0.4)和阳离子交换容量(3.8 +/- 0.7对1.6 +/- 0.4 cmol(c)kg(-1))。由于种植盆地仅占该地区的9.3%,因此与外部盆地相比,SOC的绝对增长率为0.05 t C ha(-1)yr(-1)。这对应于土壤上部20 cm的整体相对增加2.95%SOC yr(-1)。此外,热水可提取碳(HWEC)是不稳定有机物的替代物,其潜在的硝化速率始终高于外部盆地。 SOC数量和质量的显着提高可能归因于根系的增加,由于肥料和石灰的投入而有利于植物生长的条件以及盆地中雨水的渗透增加。 (c)2019 Elsevier B.V.保留所有权利。

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