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Negative effects of urbanization on agricultural soil easily oxidizable organic carbon down the profile of the Chengdu Plain, China
Author(s) -
Luo Youlin,
Li Qiquan,
Wang Changquan,
Li Bing,
Stomph TjeerdJan,
Yang Juan,
Tao Qi,
Yuan Shu,
Tang Xiaoyan,
Ge Jinru,
Yu Xuelian,
Peng Yueyue,
Xu Qiang,
Zheng Gangxun
Publication year - 2019
Publication title -
land degradation and development
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.403
H-Index - 81
eISSN - 1099-145X
pISSN - 1085-3278
DOI - 10.1002/ldr.3458
Subject(s) - urbanization , megacity , stock (firearms) , soil carbon , socioeconomic status , environmental science , land use , geography , china , context (archaeology) , agriculture , soil science , soil water , population , ecology , environmental health , biology , medicine , archaeology
Soil easily oxidizable organic carbon (EOC) is directly related to CO 2 density; dynamics in subsurface EOC have been observed globally in relation to rapid urbanization. However, in the context of rapid urbanization, the factors related to EOC and the response of the EOC pool to urbanization down the profile remain elusive. The aim of the current paper is to investigate possible changes in the distribution of EOC over the soil profile and the impact of land use, socioeconomic, and natural factors on these. The study used samples from 182 soil profiles (0–100 cm) taken in the peri‐urban areas of the megacity Chengdu (a typical megacity with rapid urbanization). Main drivers of changes in soil EOC were analyzed by using spatial and regression analyses. Closer to the centre of the city, soil EOC levels were lower and land‐use factors and socioeconomic factors contributed more to explaining variation in EOC levels in the 0–40‐cm layer, whereas natural factors were most important at larger distance from the city. The effect of land‐use factors and socioeconomic factors on EOC reached down to 60‐cm depths. Moreover, an estimated 20% loss of EOC stock was observed close to the city in comparison with the surroundings, suggesting that the rapid process of urbanization was accompanied by a loss of EOC stock down the profile to depths of 60 cm, and the negative effects on EOC stock became more intensive as the distance to the city decreased.