Soil Respiration in Semiarid Temperate Grasslands under Various Land Management

PLoS One. 2016 Jan 25;11(1):e0147987. doi: 10.1371/journal.pone.0147987. eCollection 2016.

Abstract

Soil respiration, a major component of the global carbon cycle, is significantly influenced by land management practices. Grasslands are potentially a major sink for carbon, but can also be a source. Here, we investigated the potential effect of land management (grazing, clipping, and ungrazed enclosures) on soil respiration in the semiarid grassland of northern China. Our results showed the mean soil respiration was significantly higher under enclosures (2.17 μmol.m(-2).s(-1)) and clipping (2.06 μmol.m(-2).s(-1)) than under grazing (1.65 μmol.m-(2).s(-1)) over the three growing seasons. The high rates of soil respiration under enclosure and clipping were associated with the higher belowground net primary productivity (BNPP). Our analyses indicated that soil respiration was primarily related to BNPP under grazing, to soil water content under clipping. Using structural equation models, we found that soil water content, aboveground net primary productivity (ANPP) and BNPP regulated soil respiration, with soil water content as the predominant factor. Our findings highlight that management-induced changes in abiotic (soil temperature and soil water content) and biotic (ANPP and BNPP) factors regulate soil respiration in the semiarid temperate grassland of northern China.

Publication types

  • Research Support, Non-U.S. Gov't

MeSH terms

  • Conservation of Natural Resources*
  • Ecosystem*
  • Mongolia
  • Poaceae*
  • Soil*

Substances

  • Soil

Grants and funding

This study was financially supported by the National Key Basic Research Development Program of China (2014CB138806), the International Science and Technology Cooperation Project of China (2013DFR30760), Natural Science Foundation Committee of Inner Mongolia (program no. ZD201502), National Science Foundation for Young Scientists of China (41401264), Natural Science Foundation of Inner Mongolia (2015BS0330), the Program of the National Natural Science Foundation of China (D010503).