Drought effects on soil carbon and nitrogen dynamics in global natural ecosystems

被引:259
作者
Deng, Lei [1 ,2 ]
Peng, Changhui [3 ]
Kim, Dong-Gill [4 ]
Li, Jiwei [2 ]
Liu, Yulin [2 ]
Hai, Xuying [1 ]
Liu, Qiuyu [3 ]
Huang, Chunbo [5 ]
Shangguan, Zhouping [1 ,2 ]
Kuzyakov, Yakov [6 ,7 ,8 ]
机构
[1] Northwest A&F Univ, Inst Soil & Water Conservat, State Key Lab Soil Eros & Dryland Farming Loess P, Yangling 712100, Shaanxi, Peoples R China
[2] Chinese Acad Sci & Minist Water Resources, Inst Soil & Water Conservat, Yangling 712100, Shaanxi, Peoples R China
[3] Univ Quebec Montreal, Dept Biol Sci, Ctr CEF ESCER, Montreal, PQ H3C 3P8, Canada
[4] Hawassa Univ, Wondo Genet Coll Forestry & Nat Resources, POB 128, Shashemene, Ethiopia
[5] China Univ Geosci, Sch Geog & Informat Engn, Wuhan, Peoples R China
[6] Georg August Univ, Dept Agr Soil Sci, Dept Soil Sci Temperate Ecosyst, Gottingen, Germany
[7] Kazan Fed Univ, Inst Environm Sci, Kazan, Russia
[8] RUDN Univ, Agrotechnol Inst, Moscow 117198, Russia
基金
中国国家自然科学基金;
关键词
mineral N; N mineralization; nitrification; precipitation reduction; plant C input; soil microorganisms; soil organic C; soil CO2 emission; N-MINERALIZATION; THROUGHFALL MANIPULATION; TERRESTRIAL ECOSYSTEMS; MICROBIAL ACTIVITY; SUMMER DROUGHT; CLIMATE-CHANGE; WATER PULSES; ELEVATED CO2; RESPONSES; PRECIPITATION;
D O I
10.1016/j.earscirev.2020.103501
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
Extreme droughts have serious impacts on the pools, fluxes and processes of terrestrial carbon (C) and nitrogen (N) cycles. A deep understanding is necessary to explore the impacts of this extreme climate change events. To investigate how soil C and N pools and fluxes respond to drought and explore their mechanisms we conducted a meta-analysis synthesizing the responses of soil C and N cycles to droughts (precipitation reduction experiments) in three main natural ecosystems: forests, shrubs and grasslands. Data were collected from 148 recent publications (1815 sampling data at 134 sites) with the drought experiments from 1 to 13 years across the globe. Drought reduced soil organic C content (-3.3%) mainly because of decreased plant litter input (-8.7%) and reduced litter decomposition (-13.0%) across all the three ecosystem types in the world. Drought increased mineral N content (+31%) but reduced N mineralization rate (-5.7%) and nitrification rate (-13.8%), and thus left total N unchanged. Compared with the local precipitation, drought increased the accumulation of dissolved organic C and N contents by +59% and +33%, respectively, due to retarded mineralization and higher stability of dissolved organic matter. Among the three ecosystem types, forest soils strongly increased litter C (+64%, n=8) and N content (+33%, n=6) as well as microbial CO2 (+16%, n=55), whereas total CO2 emission remains unaffected. Drought decreased soil CO2 emission (-15%, n=53) in shrubs due to reduction of microbial respiration and decreased root biomass. The 98% (n=39) increase of NH4+ concentration in forest soils corresponds to 11% (n=37) decrease of NO3- and so, it reflected the increase of N mineralization rate, but the decrease of nitrification. For shrubs and grasslands, however, stabilized or decreased N mineralization and nitrification mean less N uptake by plants under drought. Overall, the effects of drought on soil C and N cycles were regulated by the ecosystem type, drought duration and intensity. The drought intensity and duration intensify all effects, especially on the decreasing total (CO2) emission. However, the most studies mainly focused on the short-term droughts, and there is a lack of comprehensive understanding of how drought effects in a long-term consequences. So, future studies should strengthen drought frequency impacts on ecosystem C and N dynamics in the long-term sequence (> 10 years) in order to face the impacts of global change.
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页数:15
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