Increased precipitation enhances soil respiration in a semi-arid grassland on the Loess Plateau, China

Yutao Wang; Yingzhong Xie; Gillian Rapson; Hongbin Ma; Le Jing; Yi Zhang; Juan Zhang; Jianping Li

doi:10.7717/peerj.10729

Increased precipitation enhances soil respiration in a semi-arid grassland on the Loess Plateau, China

PeerJ. 2021 Feb 2:9:e10729. doi: 10.7717/peerj.10729. eCollection 2021.

Authors

Yutao Wang¹, Yingzhong Xie¹, Gillian Rapson², Hongbin Ma¹, Le Jing¹, Yi Zhang¹, Juan Zhang¹, Jianping Li¹

Affiliations

¹ School of Agriculture, Ningxia University, Yinchuan, Ningxia, China.
² School of Agriculture and Environment, Massey University, Palmerston North, New Zealand.

Abstract

Background: Precipitation influences the vulnerability of grassland ecosystems, especially upland grasslands, and soil respiration is critical for carbon cycling in arid grassland ecosystems which typically experience more droughty conditions.

Methods: We used three precipitation treatments to understand the effect of precipitation on soil respiration of a typical arid steppe in the Loess Plateau in north-western China. Precipitation was captured and relocated to simulate precipitation rates of 50%, 100%, and 150% of ambient precipitation.

Results and discussion: Soil moisture was influenced by all precipitation treatments. Shoot biomass was greater, though non-significantly, as precipitation increased. However, both increase and decrease of precipitation significantly reduced root biomass. There was a positive linear relationship between soil moisture and soil respiration in the study area during the summer (July and August), when most precipitation fell. Soil moisture, soil root biomass, pH, and fungal diversity were predictors of soil respiration based on partial least squares regression, and soil moisture was the best of these.

Conclusion: Our study highlights the importance of increased precipitation on soil respiration in drylands. Precipitation changes can cause significant alterations in soil properties, microbial fungi, and root biomass, and any surplus or transpired moisture is fed back into the climate, thereby affecting the rate of soil respiration in the future.

Keywords: Climate change; Loess Plateau; Precipitation; Respiration; Soil respiration; Typical steppe.

Grants and funding

This study was financially supported by the Research and Development Project of Ningxia (2020BEG03046), Natural Science Foundation of Ningxia (2019AAC03042), and Top Discipline Construction Project of Pratacultural Science (NXYLXK2017A01). The funders had no role in study design, data collection and analysis, decision to publish, or preparation of the manuscript.