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Size and dynamics of soil organic carbon stock in cropland of the Eastern Qinghai-Tibetan Plateau

机译:青藏高原东部农田土壤有机碳储量的大小和动态

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摘要

Estimating the size and changes in cropland soil organic carbon (SOC) stock in the Qinghai-Tibetan Plateau is important for the improvement of soil quality and mitigation of greenhouse gas emissions in this region. In this study, we investigated the dynamics of SOC concentrations, SOC density (SOCD), and SOC stock in cropland topsoil (0-20 cm) in the eastern Qinghai Province from the 1980s (1980-1989) to recent years (2000-2014). We conducted a long-term fertilization field experiment initiated in 1992 in eastern agricultural region of the Plateau, and used additional data of Qinghai section collected in 1980s by the Second State Soil Survey of China (SSSSC), observational data obtained from field studies in the area from 2006 to 2007. The results showed that the average SOC concentration during 2006-2007 increased by 16.0% compared to that in the 1980s, and increased by 11.9-24.1% in the treatments of the long-term field experiment in 2014 compared to that in 1992. Up until the 1980s, 21.9 Tg SOC was stored in 711751.6 ha of topsoil throughout the entire cropland region. The average SOCD in Huangzhong County during 2006-2007 was 35.4 Mg ha(-1), 9.7% higher than that during 1980-1989 (32.3 Mg ha(-1)). The annual rate of increase in SOCD ranged from 0.10 to 0.41 Mg ha(-1) yr-lin the long-term chemical fertilization treatments and from 0.22 to 0.85 Mg ha(-1) yr-lin the combined long-term straw return and chemical fertilization treatments. The order of the soil types in the region with respect to mean SOC concentration was Chernozems > Gleysols >Anthrosols > Luvisols > Cambisols > Kastanozems > Calcisols. The long-term field experiment verified the increase of SOC stock per unit area in the whole region. Organic fertilization, especially straw return and chemical fertilization and other management strategies such as conservation tillage, contributed to the increase of the SOC stock. This study provides an understanding of SOC size and dynamics in cropland of Qinghai-Tibetan Plateau and highlights the importance of protecting cropland and using straw return to improve management practices and increase the SOC stock in cropland of the plateau. (C) 2016 Elsevier B.V. All rights reserved.
机译:估算青藏高原农田土壤有机碳(SOC)储量的大小和变化,对于改善该地区的土壤质量和减少温室气体排放至关重要。在这项研究中,我们调查了1980年代(1980-1989)至近几年(2000-2014)青海省东部农田表层土壤(0-20 cm)中SOC浓度,SOC密度(SOCD)和SOC储量的动态。 )。我们于1992年在高原东部农业地区进行了长期的施肥田间试验,并使用了1980年代由中国第二次土壤调查(SSSSC)收集的青海剖面的其他数据,这些数据来自于该州的田间研究。结果表明,从2006年到2007年,该地区的平均SOC浓度比1980年代增加了16.0%,与2014年相比,与2014年代相比,2014年的长期野外试验处理的平均SOC浓度增加了11.9-24.1%。直到1992年代。在整个农田地区,表土中的711.91.6公顷中储存了21.9 Tg SOC。 Huang中县2006-2007年的平均SOCD为35.4 Mg ha(-1),比1980-1989年的32.3 Mg ha(-1)高9.7%。长期化学施肥处理后SOCD的年增长率在0.10至0.41 Mg ha(-1)yr-lin之间,而长期秸秆还田和回灌的总和从0.22至0.85 Mg ha(-1)yr-lin之间。化学施肥处理。相对于平均SOC浓度,该地区土壤类型的顺序为黑钙土>斜ley>人为土> Luvisols>坎比索尔> Kastanozems>钙土。长期的野外实验证实了整个区域每单位面积SOC储量的增加。有机施肥,特别是秸秆还田和化学施肥,以及诸如耕作耕作的其他管理策略,促进了SOC的增加。该研究提供了对青藏高原农田土壤有机碳的大小和动态的理解,并强调了保护耕地和利用秸秆还田来改善管理实践和增加高原农田土壤有机碳储量的重要性。 (C)2016 Elsevier B.V.保留所有权利。

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