Title Higher soil acidification risk in southeastern Tibetan Plateau
Authors Zhang, Qiongyu
Wang, Qiufeng
Zhu, Jianxing
Xu, Li
Li, Mingxu
Rengel, Zed
Xiao, Jingfeng
Hobbie, Erik A.
Piao, Shilong
Luo, Wentao
He, Nianpeng
Affiliation Chinese Acad Sci, Key Lab Ecosyst Network Observat & Modeling, Inst Geog Sci & Nat Resources Res, Beijing 100101, Peoples R China
Univ Chinese Acad Sci, Coll Resources & Environm, Beijing 100049, Peoples R China
Univ Western Australia, Sch Agr & Environm, Soil Sci & Plant Nutr, Perth, WA 6009, Australia
Inst Adriat Crops & Karst Reclamat, Split 21000, Croatia
Univ New Hampshire, Inst Study Earth Oceans & Space, Earth Syst Res Ctr, Durham, NH 03824 USA
Peking Univ, Coll Urban & Environm Sci, Sino French Inst Earth Syst Sci, Beijing, Peoples R China
Chinese Acad Sci, Inst Appl Ecol, State Key Lab Forest & Soil Ecol, Shenyang 110164, Peoples R China
Northeast Normal Univ, Inst Grassland Sci, Changchun 130024, Peoples R China
Minist Educ, Key Lab Vegetat Ecol, Changchun 130024, Peoples R China
Keywords PERSISTENT ORGANIC POLLUTANTS
NITROGEN DEPOSITION
SPATIAL-DISTRIBUTION
PROTON SOURCES
BASE CATIONS
CHINA
AIR
PH
CLIMATE
ECOSYSTEMS
Issue Date 10-Feb-2021
Publisher SCIENCE OF THE TOTAL ENVIRONMENT
Abstract Stable soil pH is a key property in maintaining an ecosystem's structure, function, and sustainability. Increasing atmospheric deposition and grassland use on the Tibetan Plateau (TP) may increase the soil acidification risk, but we lack such information to date. Here, we evaluated the soil acidification risk in the TP, by comparing it with that in the Mongolia Plateau (MP) and applying the acid-base balance principles on atmospheric inputs, soils, and plants from 1980 to 2019. Cumulative acid input was lower in the TP than in the MP. Sulfur contributed more to acidity than nitrogen and atmospheric deposition contributed more to acidity than grassland use. Acid input was mainly influenced by local industry, animal husbandry and transportation in the MP, while in the TP it was also affected by the long-distance transportation of pollutants from South Asia and southern China. Overall, the TP was less acid-sensitive than the MP because of higher inorganic carbon content. However, soils in the southeastern TP, covering 21% of the total area, were acid-sensitive due to low levels of soil exchangeable base cation (EBCs) and lack of calcium carbonate. Coincidentally, the southeastern region has the highest concentration of acid input in the TP due to more rapid development and stronger influence of adjacent high acid deposition regions than others. Therefore, the acidification risk to the southeastern region is much higher than to other regions of the TP and the MP; in this region, the EBCs are likely to be depleted approximately 95 years earlier than in the MP. The findings of this study provide insights into the response of the TP to global change. For the ecosystem sustainability of southeastern TP, control of atmospheric acid deposition, especially sulfur deposition, in both local and adjacent regions and nations is required. (c) 2020 The Authors. Published by Elsevier B.V.
URI http://hdl.handle.net/20.500.11897/603106
ISSN 0048-9697
DOI 10.1016/j.scitotenv.2020.143372
Indexed SCI(E)
Appears in Collections: 城市与环境学院

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