Soil respiration response to alterations in precipitation and nitrogen addition in a desert steppe in northern China

被引:28
|
作者
Wang, Zhen [1 ]
Mckenna, Thomas P. [2 ]
Schellenberg, Michael P. [3 ]
Tang, Shiming [4 ]
Zhang, Yujuan [1 ]
Ta, Na [1 ]
Na, Risu [1 ]
Wang, Hai [1 ]
机构
[1] Chinese Acad Agr Sci, Grassland Res Inst, Hohhot 010010, Peoples R China
[2] Univ Kansas, Kansas Biol Survey, Dept Ecol & Evolutionary Biol, Lawrence, KS 66047 USA
[3] AAFC AAC, SCRDC, Box 1030, Swift Current, SK S9H 3X2, Canada
[4] Inner Mongolia Univ, Dept Ecol, Sch Ecol & Environm, 235 West Coll Rd, Hohhot 010021, Peoples R China
基金
中国国家自然科学基金;
关键词
Grass; Forb; Soil water content; Net primary productivity; Soil total nitrogen content; MICROBIAL RESPIRATION; SEMIARID GRASSLANDS; ROOT RESPIRATION; WATER PULSES; CO2; FLUXES; PLANT; CARBON; FERTILIZATION; TEMPERATURE; ECOSYSTEM;
D O I
10.1016/j.scitotenv.2019.05.419
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Global climate change is expected to significantly influence soil respiration. When limited, rainfall and nitrogen (N) deposition strongly modify soil respiration in a broad range of biomes, but uncertainty remains with regards to the influence of the interactions of seasonal rainfall distribution and N deposition on soil respiration in an arid steppe. In the present study, we manipulated precipitation using V-shaped plexiglass gutters (minus 50%, control, and plus 50% treatments) and tested various N additions (control and plus 35 kg N ha(-1) yr(-1)) to evaluate their impact on soil respiration, measured using a Li-Cor 8100, in a desert steppe in China. Increased precipitation stimulated soil respiration by 26.1%, while decreased precipitation significantly reduced soil respiration by 10.8%. There was a significant increase in soil respiration under N addition at 11.5%. Statistical assessment of their interactions demonstrated that N supplementation strengthened the stimulation of soil respiration under increased precipitation, whereas decreased precipitation offset the positive impact of N addition and led to a reduction in soil respiration. Contrasting interannual precipitation patterns strongly influenced the temporal changes in soil respiration as well as its response to N addition, indicating that the desert steppe plant community was co-limited by water and N. Net primary productivity (aboveground and belowground) predominantly drove soil respiration under altered precipitation and N addition. As grasses are better equipped for water deficit due to their previous exposure to long periods without water, there could be a shift from forb to grass communities under drier conditions. These findings highlight the importance of assessing the differential impacts of plant traits and soil physiochemical properties on soil respiration under altered precipitation and N addition. (C) 2019 Published by Elsevier B.V.
引用
收藏
页码:231 / 242
页数:12
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