Landscape Ecology

, Volume 30, Issue 9, pp 1683–1699 | Cite as

Predominant control of moisture on soil organic carbon mineralization across a broad range of arid and semiarid ecosystems on the Mongolia plateau

  • Jia Mi
  • Jianjun Li
  • Dima Chen
  • Yichun Xie
  • Yongfei BaiEmail author
Research Article


Soil moisture and temperature are known to be the two environmental constraints regulating mineralization of soil organic carbon (SOC). However, it remains unclear to what extent the moisture, temperature, and other abiotic and biotic factors affect the mineralization of SOC across broad geographic regions. Here, we examined the effects of multiple abiotic and biotic factors on SOC mineralization across 12 widespread arid and semiarid ecosystems on the Mongolia plateau, by using an integrative approach combining short-term laboratory incubations (28-day), field survey, and structure equation modeling (SEM). Our results showed that soil moisture had a predominant control on SOC mineralization across all sites. The average CO2 emissions over all sites increased by 23 % from 30 to 60 % water filled pore space (WFPS) and by 176 % from 60 to 90 % WFPS. Under conditions of 25 °C and 60 % WFPS, the cumulative CO2–C emissions in the topsoil (0–20 cm) diminished in the following order: meadow steppe (227 mg kg−1) > typical steppe (216 mg kg−1) > desert (99 mg kg−1) > desert steppe (72 mg kg−1). The temperature sensitivity of SOC mineralization (Q10), the proportional change in carbon mineralization rate given a 10 °C temperature gradient, was highest under conditions of low temperature and high moisture, but it was lowest under high temperature and low moisture. The SEM analyses demonstrate that the mineralization potential of SOC seems to be directly regulated by microbe activity and substrate availability. Climatic factors (e.g. mean annual precipitation, mean annual temperature), above- and belowground biomass, and soil pH, which regulate SOC and microbial biomass carbon content, also indirectly influence the SOC mineralization. Our results indicate that global climate change, particularly the increase in the frequency of extreme storms and droughts, will substantially affect SOC mineralization and ecosystem carbon cycle in arid and semiarid regions.


SOC mineralization Precipitation gradient Water filled pore space (WFPS) Temperature sensitivity of SOC mineralization Microbial biomass carbon 



We are grateful to Tao Sang for comments on an early version of this manuscript. We thank Hongwei Wan and Junhui Cheng for their helps with statistical analysis. We also gratefully acknowledge undergraduate students from the Inner Mongolia Agriculture University for their helps with fieldwork. This project was supported by the Natural Science Foundation of China (31030013, 31320103916), Strategic Priority Research Program of the Chinese Academy of Sciences (XDA05050400), and Land-Cover/Land-Use Program at NASA (Grant No. NNX09AK87G).

Supplementary material

10980_2014_40_MOESM1_ESM.docx (632 kb)
Supplementary material 1 (DOCX 631 kb)


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Copyright information

© Springer Science+Business Media Dordrecht 2014

Authors and Affiliations

  • Jia Mi
    • 1
  • Jianjun Li
    • 1
  • Dima Chen
    • 1
  • Yichun Xie
    • 2
  • Yongfei Bai
    • 1
    Email author
  1. 1.State Key Laboratory of Vegetation and Environmental Change, Institute of BotanyChinese Academy of SciencesBeijingPeople’s Republic of China
  2. 2.Department of Geography and GeologyEastern Michigan UniversityYpsilantiUSA

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