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青藏高原三江源地区高寒草原土壤有机碳储量及其不确定性

Alpine grassland soil organic carbon stock and its uncertainty in the three rivers source region of the Tibetan Plateau.

作者信息

Chang Xiaofeng, Wang Shiping, Cui Shujuan, Zhu Xiaoxue, Luo Caiyun, Zhang Zhenhua, Wilkes Andreas

机构信息

State Key Laboratory of Soil Erosion and Dryland Farming on Loess Plateau, Institute of Soil and Water Conservation, Northwest A&F University, Yangling, China; Key Laboratory of Adaptation and Evolution of Plateau Biota, Northwest Institute of Plateau Biology, Chinese Academy of Science, Xining, China.

Laboratory of Alpine Ecology and Biodiversity, Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing, China.

出版信息

PLoS One. 2014 May 12;9(5):e97140. doi: 10.1371/journal.pone.0097140. eCollection 2014.

Abstract

Alpine grassland of the Tibetan Plateau is an important component of global soil organic carbon (SOC) stocks, but insufficient field observations and large spatial heterogeneity leads to great uncertainty in their estimation. In the Three Rivers Source Region (TRSR), alpine grasslands account for more than 75% of the total area. However, the regional carbon (C) stock estimate and their uncertainty have seldom been tested. Here we quantified the regional SOC stock and its uncertainty using 298 soil profiles surveyed from 35 sites across the TRSR during 2006-2008. We showed that the upper soil (0-30 cm depth) in alpine grasslands of the TRSR stores 2.03 Pg C, with a 95% confidence interval ranging from 1.25 to 2.81 Pg C. Alpine meadow soils comprised 73% (i.e. 1.48 Pg C) of the regional SOC estimate, but had the greatest uncertainty at 51%. The statistical power to detect a deviation of 10% uncertainty in grassland C stock was less than 0.50. The required sample size to detect this deviation at a power of 90% was about 6-7 times more than the number of sample sites surveyed. Comparison of our observed SOC density with the corresponding values from the dataset of Yang et al. indicates that these two datasets are comparable. The combined dataset did not reduce the uncertainty in the estimate of the regional grassland soil C stock. This result could be mainly explained by the underrepresentation of sampling sites in large areas with poor accessibility. Further research to improve the regional SOC stock estimate should optimize sampling strategy by considering the number of samples and their spatial distribution.

摘要

青藏高原的高寒草原是全球土壤有机碳(SOC)储量的重要组成部分,但实地观测不足以及较大的空间异质性导致其估算存在很大不确定性。在三江源地区(TRSR),高寒草原占总面积的75%以上。然而,该区域碳(C)储量估算及其不确定性很少得到检验。在此,我们利用2006 - 2008年期间在TRSR地区35个地点调查的298个土壤剖面,对区域SOC储量及其不确定性进行了量化。我们发现,TRSR高寒草原的上层土壤(0 - 30厘米深度)储存了2.03Pg C,其95%置信区间为1.25至2.81Pg C。高寒草甸土壤占区域SOC估算的73%(即1.48Pg C),但不确定性最大,为51%。检测草地C储量10%不确定性偏差的统计功效小于0.50。在功效为90%时检测此偏差所需的样本量比所调查的样本点数多约6 - 7倍。将我们观测到的SOC密度与Yang等人数据集中的相应值进行比较表明,这两个数据集具有可比性。合并后的数据集并未降低区域草地土壤C储量估算的不确定性。这一结果主要可以通过难以到达的大面积区域采样点代表性不足来解释。为改进区域SOC储量估算的进一步研究应通过考虑样本数量及其空间分布来优化采样策略。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/4357/4018262/f54bcee09db7/pone.0097140.g001.jpg

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