首页> 外文期刊>Agriculture, Ecosystems & Environment: An International Journal for Scientific Research on the Relationship of Agriculture and Food Production to the Biosphere >Previous land use and climate influence differences in soil organic carbon following reforestation of agricultural land with mixed-species plantings
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Previous land use and climate influence differences in soil organic carbon following reforestation of agricultural land with mixed-species plantings

机译:农林混种种植造林后土壤有机碳的先前土地利用和气候影响差异

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摘要

Reforestation of agricultural land with mixed-species environmental plantings (native trees and shrubs) can contribute to mitigation of climate change through sequestration of carbon. Although soil carbon sequestration following reforestation has been investigated at site- and regional-scales, there are few studies across regions where the impact of a broad range of site conditions and management practices can be assessed. We collated new and existing data on soil organic carbon (SOC, 0-30 cm depth, N = 117 sites) and litter (N = 106 sites) under mixed-species plantings and an agricultural pair or baseline across southern and eastern Australia. Sites covered a range of previous land uses, initial SOC stocks, climatic conditions and management types. Differences in total SOC stocks following reforestation were significant at 52% of sites, with a mean rate of increase of 0.57 +/- 0.06 Mg C ha(-1) y(-1). Increases were largely in the particulate fraction, which increased significantly at 46% of sites compared with increases at 27% of sites for the humus fraction. Although relative increase was highest in the particulate fraction, the humus fraction was the largest proportion of total SOC and so absolute differences in both fractions were similar. Accumulation rates of carbon in litter were 0.39 +/- 0.02 Mg C ha(-1)y(-1), increasing the total (soil + litter) annual rate of carbon sequestration by 68%. Previously-cropped sites accumulated more SOC than previously-grazed sites. The explained variance differed widely among empirical models of differences in SOC stocks following reforestation according to SOC fraction and depth for previously-grazed (R-2 = 0.18-0.51) and previously-cropped (R-2 = 0.14-0.60) sites. For previously-grazed sites, differences in SOC following reforestation were negatively related to total SOC in the pasture. By comparison, for previously cropped sites, differences in SOC were positively related to mean annual rainfall. This improved broad scale understanding of the magnitude and predictors of changes in stocks of soil and litter C following reforestation is valuable for the development of policy on carbon markets and the establishment of future mixed-species environmental plantings. (C) 2016 Elsevier B.V. All rights reserved.
机译:通过混合种环境植物(本地树木和灌木)对农业用地进行重新造林,可以通过固碳来缓解气候变化。尽管已经在站点和区域范围内对造林后的土壤碳固存进行了研究,但跨区域的研究很少,可以评估各种站点条件和管理实践的影响。我们整理了澳大利亚南部和东部地区混合物种种植和农业对或基线下土壤有机碳(SOC,0-30厘米深度,N = 117个地点)和凋落物(N = 106个地点)的新数据和现有数据。地点涵盖了以前的土地用途,初始SOC存量,气候条件和管理类型。造林后总SOC存量的差异在52%的站点上是显着的,平均增长率为0.57 +/- 0.06 Mg C ha(-1)y(-1)。颗粒部分的增加很大,与腐殖质部分相比,在46%的位置显着增加,而在27%的位置增加。尽管相对增加在微粒部分中最高,但腐殖质部分是总SOC的最大部分,因此两个部分的绝对差异相似。凋落物中的碳累积速率为0.39 +/- 0.02 Mg C ha(-1)y(-1),使总的(土壤+凋落物)年固碳率提高了68%。以前种植的站点比以前种植的站点累积了更多的SOC。在重新造林后,SOC储量差异的经验模型之间的差异很大,这取决于先前放牧(R-2 = 0.18-0.51)和先前耕种(R-2 = 0.14-0.60)地点的SOC分数和深度。对于先前放牧的地点,重新造林后SOC的差异与牧场中的总SOC呈负相关。相比之下,对于以前种植的地点,SOC的差异与年平均降水量呈正相关。植树造林后对土壤和凋落物C储量变化的幅度和预测因子的广泛了解,对于制定碳市场政策和建立未来的混合物种环境种植园非常有用。 (C)2016 Elsevier B.V.保留所有权利。

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