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Chinese Journal of Applied Ecology ›› 2019, Vol. 30 ›› Issue (3): 913-922.doi: 10.13287/j.1001-9332.201903.011

• Research paper • Previous Articles     Next Articles

Dynamic and its driving factors of soil potential acid in croplands of Fujian Province, China

ZHOU Jie-ying1, ZHANG Li-ming1,2, YANG Wen-hao1,2, ZHOU Bi-qing1,2, XING Shi-he1,2*   

  1. 1College of Resources and Environment, Fujian Agricultural and Forestry University, Fuzhou 350002, China;
    2University Key Lab of Soil Ecosystem Health and Regulation in Fujian, Fuzhou 350002, China
  • Received:2018-08-13 Online:2019-03-20 Published:2019-03-20
  • Supported by:
    This work was supported by the Project of Cropland Quality Improvement, Ministry of Agriculture and Rural Affairs of People’s Republic of China (20170011).

Abstract: Soil potential acid is one of the potential factors limiting plant growth, and also an important base in soil acidity regulation. The potential acid and pH value of surface soil samples of cultivated lands in Fujian Province were proportionally selected and measured, and then the optimized relational model between soil pH and potential acid value was fitted. The 1:50 000 databases of cropland soil potential acid in 1982, 2008 and 2016 were established by using the topsoil pH data of 36777, 236445 and 21269 sampling sites collected in 1982, 2008 and 2016 respectively. The dynamics of cropland soil potential acid in Fujian Province and its driving factors were explored by the integrative method of GIS and grey correlation analysis. The results showed that the quantities of soil potential acid in cropland generally increased in Fujian Province from 1982 to 2016. Compared with 1982, the averages of soil potential acid in 2008 and 2016 increased 1.30 and 1.49 cmol·kg-1, respectively. The increase rate of soil potential acid from 1982 to 2008 was 0.03 cmol·kg-1·a-1 higher than that from 2008 to 2016. Meanwhile, the changes of cropland soil potential acid showed significant spatial difference. The change of cropland soil potential acid in Sanming was minimum, and the change in Longyan was maximum, being four times higher than that in Sanming. The change of soil potential acid in different use types of cropland was following the order: paddy field > irrigated land > dry land. The changes of soil potential acid in acid sulfate paddy soils, gleyed paddy soils and submergenic paddy soils were maximum, which were one time higher than the mean change across the whole Province, while the changes in latosolic red earths and salinized paddy soils were minimum, which were 25.7% and 28.4% of the mean change in the Province, respectively. The driving factors for the dynamics of cropland soil potential acid in Fujian Province included the application rates of nitrogen and phosphorus fertilizer, cation exchange capacity (CEC), clay content, pH and silt content, with grey correlation coefficient (absolute value) being higher than 0.92. Accordingly, it would be an effective approach to slow down the increase of cropland soil potential acid in Fujian Province to optimize fertilization management and apply alkaline ameliorant scientifically.

Key words: cropland, grey relational analysis, potential acid, GIS