中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Hydrothermal conditions determine soil potential net N mineralization rates in arid and semi-arid grasslands

文献类型:期刊论文

作者Hu, Shuya1,2; Wang, Changhui1,3; Risch, Anita C.4; Liu, Yuan5; Li, Yang1,2; Li, Lei1,2; Xu, Xiaohui1,2; He, Nianpeng2,5; Han, Xingguo1,2; Huang, Jianhui1,2
刊名FUNCTIONAL ECOLOGY
出版日期2022-09-12
页码10
ISSN号0269-8463
关键词desert steppe grassland hydrothermal condition meadow steppe soil net N mineralization transects typical steppe
DOI10.1111/1365-2435.14167
通讯作者Wang, Changhui(wangch@ibcas.ac.cn) ; Huang, Jianhui(jhhuang@ibcas.ac.cn)
英文摘要Soil net nitrogen (N) mineralization is a key biogeochemical process influencing plant available N and net primary productivity in terrestrial ecosystems. However, the spatial variations and controlling factors of soil net N mineralization (R-PNM) in arid and semi-arid grasslands are less studied and unclear. In this study, we investigated the soil R-PNM by performing a laboratory incubation experiment. Soil samples were collected from 30 sites in three east-west transects on the Inner Mongolia Plateau (MP), Loess Plateau (LP) and Tibetan Plateau (TP) along a 3200 km arid and semi-arid grassland gradient, with each transect containing three different grassland types (meadow steppe [MS], typical steppe [TS] and desert steppe [DS], respectively). Results showed that the average R-PNM values ranged from -0.37 to 1.29 mg N kg(-1) day(-1), with a significantly lower R-PNM found in the DS (0.08 +/- 0.01 mg N kg(-1) day(-1)) compared with those in the MS (0.30 +/- 0.03 mg N kg(-1) day(-1)) and in the TS (0.33 +/- 0.03 mg N kg(-1) day(-1)) in the MP and LP transects (p < 0.05). This difference could be explained by variations in climatic and soil factors, such as hydrothermal index (HT), the soil pH, soil organic matter (SOM) and precipitation. However, no significant differences in R-PNM were found among different grassland types in the TP transect, possibly due to the similarly low microbial activity, as indicated by the microbial biomass carbon values. Across all three grassland transects, HT, SOM and microbial variables were the major factors controlling R-PNM, which together explained 20.7% of the variation in R-PNM. Further structural equation model analysis indicated HT was an integral predictor of R-PNM, directly or indirectly via SOM, under different conditions of precipitation and temperature. Our findings provide field evidence and parameters for biogeochemical cycling to better predict future N transformation processes under changing precipitation and temperature regimes across a wide range of arid and semi-arid grassland ecosystems. Read the free Plain Language Summary for this article on the Journal blog.
WOS关键词NITROGEN MINERALIZATION ; MICROBIAL BIOMASS ; TEMPERATURE SENSITIVITY ; EXTRACTION METHOD ; TYPICAL STEPPE ; PADDY SOILS ; CARBON ; WATER ; AVAILABILITY ; RESPIRATION
资助项目Strategic Priority Research Program of Chinese Academy of Sciences[XDA23080402] ; Second Tibetan Plateau Scientific Expedition and Research Program (STEP)[2019QZKK0606] ; Chinese National Key Development Program for Basic Research[2017YFA0604802] ; National Natural Science Foundation of China[31770526] ; High-Level Talents Project of Shanxi Agricultural University[2021XG008] ; Shanxi Key Laboratory Project[202104010910017]
WOS研究方向Environmental Sciences & Ecology
语种英语
出版者WILEY
WOS记录号WOS:000852983800001
资助机构Strategic Priority Research Program of Chinese Academy of Sciences ; Second Tibetan Plateau Scientific Expedition and Research Program (STEP) ; Chinese National Key Development Program for Basic Research ; National Natural Science Foundation of China ; High-Level Talents Project of Shanxi Agricultural University ; Shanxi Key Laboratory Project
源URL[http://ir.igsnrr.ac.cn/handle/311030/182820]  
专题中国科学院地理科学与资源研究所
通讯作者Wang, Changhui; Huang, Jianhui
作者单位1.Chinese Acad Sci, Inst Bot, State Key Lab Vegetat & Environm Change, Beijing, Peoples R China
2.Univ Chinese Acad Sci, Beijing, Peoples R China
3.Shanxi Agr Univ, Coll Grassland Sci, Taigu, Peoples R China
4.Swiss Fed Inst Forest Snow & Landscape Res WSL, Community Ecol, Birmensdorf, Switzerland
5.Chinese Acad Sci, Inst Geog Sci & Nat Resources Res, Key Lab Ecosyst Network Observat & Modeling, Beijing, Peoples R China
推荐引用方式
GB/T 7714
Hu, Shuya,Wang, Changhui,Risch, Anita C.,et al. Hydrothermal conditions determine soil potential net N mineralization rates in arid and semi-arid grasslands[J]. FUNCTIONAL ECOLOGY,2022:10.
APA Hu, Shuya.,Wang, Changhui.,Risch, Anita C..,Liu, Yuan.,Li, Yang.,...&Huang, Jianhui.(2022).Hydrothermal conditions determine soil potential net N mineralization rates in arid and semi-arid grasslands.FUNCTIONAL ECOLOGY,10.
MLA Hu, Shuya,et al."Hydrothermal conditions determine soil potential net N mineralization rates in arid and semi-arid grasslands".FUNCTIONAL ECOLOGY (2022):10.

入库方式: OAI收割

来源:地理科学与资源研究所

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