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农业活动导致肯尼亚表层土壤流失率升高,但梯田建设和减少耕作可以扭转这一局面。

Agricultural practices drive elevated rates of topsoil decline across Kenya, but terracing and reduced tillage can reverse this.

作者信息

Feeney Christopher J, Robinson David A, Thomas Amy R C, Borrelli Pasquale, Cooper David M, May Linda

机构信息

UK Centre for Ecology & Hydrology, Environment Centre Wales, Deiniol Road, Bangor, Gwynedd LL57 2UW, UK.

UK Centre for Ecology & Hydrology, Environment Centre Wales, Deiniol Road, Bangor, Gwynedd LL57 2UW, UK.

出版信息

Sci Total Environ. 2023 Apr 20;870:161925. doi: 10.1016/j.scitotenv.2023.161925. Epub 2023 Jan 31.

Abstract

As agricultural land area increases to feed an expanding global population, soil erosion will likely accelerate, generating unsustainable losses of soil and nutrients. This is critical for Kenya where cropland expansion and nutrient loading from runoff and erosion is contributing to eutrophication of freshwater ecosystems and desertification. We used the Revised Universal Soil Loss Equation (RUSLE) to predict soil erosion rates under present land cover and potential natural vegetation nationally across Kenya. Simulating natural vegetation conditions allows the degree to which erosion rates are elevated under current land use practices to be determined. This methodology exploits new digital soil maps and two vegetation cover maps to model topsoil (top 20 cm) erosion rates, lifespans (the mass of topsoil divided by erosion rate), and lateral nutrient fluxes (nutrient concentration times erosion rate) under both scenarios. We estimated the mean soil erosion rate under current land cover at 5.5 t ha yr, ~3 times the rate estimated for natural vegetation cover (1.8 t ha yr), and equivalent to 320 Mt yr of topsoil lost nationwide. Under present erosion rates, ~8.8 Mt, ~315 Kt, and ~ 110 Kt of soil organic carbon, nitrogen and phosphorous are lost from soil every year, respectively. Further, 5.3 % of topsoils (3.1 Mha), including at >25 % of croplands, have short lifespans (<100 years). Additional scenarios were tested that assume combinations of terracing and reduced tillage practices were adopted on croplands to mitigate erosion. Establishing bench terraces with zoned tillage could reduce soil losses by ≥75 %; up to 87.1 t ha yr. These reductions are comparable to converting croplands to natural vegetation, demonstrating most agricultural soils can be conserved successfully. Extensive long-term monitoring of croplands with terraces and reduced tillage established is required to verify the efficacy of these agricultural support practices as indicated by our modelling.

摘要

随着农业用地面积增加以养活不断增长的全球人口,土壤侵蚀可能会加速,导致土壤和养分的不可持续流失。这对肯尼亚至关重要,因为那里的农田扩张以及径流和侵蚀带来的养分负荷正在导致淡水生态系统富营养化和荒漠化。我们使用修订后的通用土壤流失方程(RUSLE)来预测肯尼亚全国目前土地覆盖和潜在自然植被下的土壤侵蚀率。模拟自然植被状况可以确定当前土地利用方式下侵蚀率升高的程度。该方法利用新的数字土壤图和两幅植被覆盖图来模拟两种情景下的表土(顶部20厘米)侵蚀率、寿命(表土质量除以侵蚀率)和侧向养分通量(养分浓度乘以侵蚀率)。我们估计目前土地覆盖下的平均土壤侵蚀率约为5.5吨/公顷·年,约为自然植被覆盖下估计侵蚀率(约1.8吨/公顷·年)的3倍,相当于全国每年损失约3.2亿吨表土。按照目前的侵蚀率,每年分别有约880万吨、31.5万吨和11万吨的土壤有机碳、氮和磷从土壤中流失。此外,5.3%的表土(约310万公顷),包括超过25%的农田,寿命较短(<100年)。还测试了其他情景,假设在农田上采用梯田和减少耕作相结合的做法来减轻侵蚀。建立带分区耕作的梯田可以减少≥75%的土壤流失;高达87.1吨/公顷·年。这些减少量与将农田转变为自然植被相当,表明大多数农业土壤可以成功得到保护。需要对建立了梯田和减少耕作的农田进行广泛的长期监测,以验证我们模型所示的这些农业支持措施的有效性。

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