Spatiotemporal Pattern of Soil Respiration of Terrestrial Ecosystems in China: The Development of a Geostatistical Model and Its Simulation

• Published in: Environmental science & technology Vol. 44; no. 16; pp. 6074 - 6080
• Main Authors: Yu, Guirui, Zheng, Zemei, Wang, Qiufeng, Fu, Yuling, Zhuang, Jie, Sun, Xiaomin, Wang, Yuesi
• Format: Journal Article
• Language: English
• Published: Washington, DC American Chemical Society 15.08.2010
• Subjects: Animal and plant ecology; Animal, plant and microbial ecology; Biological and medical sciences; Carbon; Carbon Dioxide - analysis; Characterization of Natural and Affected Environments; China; Computer Simulation; Ecosystem; Ecosystems; Environmental science; Fundamental and applied biological sciences. Psychology; General aspects. Techniques; Geostatistics; Methods and techniques (sampling, tagging, trapping, modelling...); Models, Statistical; Respiration; Simulation; Soil - analysis; Soil mechanics; Soil sciences; Synecology; Terrestrial ecosystems; Time Factors; Asia; China; Soils; Simulation model; Respiration; Spatial variation; Time variation; Geostatistics
• ISSN: 0013-936X; 1520-5851; 1520-5851
• DOI: 10.1021/es100979s

Quantification of the spatiotemporal pattern of soil respiration (R s) at the regional scale can provide a theoretical basis and fundamental data for accurate evaluation of the global carbon budget. This study summarizes the R s data measured in China from 1995 to 2004. Based on the data, a new region-scale geostatistical model of soil respiration (GSMSR) was developed by modifying a global scale statistical model. The GSMSR model, which is driven by monthly air temperature, monthly precipitation, and soil organic carbon (SOC) density, can capture 64% of the spatiotemporal variability of soil R s . We evaluated the spatiotemporal pattern of R s in China using the GSMSR model. The estimated results demonstrate that the annual R s in China ranged from 3.77 to 4.00 Pg C yr−1 between 1995 and 2004, with an average value of 3.84 ± 0.07 Pg C yr−1, contributing 3.92%−4.87% to the global soil CO2 emission. Annual R s rate of evergreen broadleaved forest ecosystem was 698 ± 11 g C m−2 yr−1, significantly higher than that of grassland (439 ± 7 g C m−2 yr−1) and cropland (555 ± 12 g C m−2 yr−1). The contributions of grassland, cropland, and forestland ecosystems to the total R s in China were 48.38 ± 0.35%, 22.19 ± 0.18%, and 20.84 ± 0.13%, respectively.