Significant Acidification in Major Chinese Croplands
Author(s) -
Jingheng Guo,
Xu Liu,
Ying Zhang,
Jianning Shen,
Wenxuan Han,
Wei Zhang,
Peter Christie,
K. W. T. Goulding,
Peter M. Vitousek,
F.S. Zhang
Publication year - 2010
Publication title -
science
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 12.556
H-Index - 1186
eISSN - 1095-9203
pISSN - 0036-8075
DOI - 10.1126/science.1182570
Subject(s) - hectare , soil acidification , soil water , environmental science , soil ph , cropping , agriculture , nitrogen , cycling , agronomy , acid rain , environmental chemistry , chemistry , soil science , geography , ecology , biology , forestry , organic chemistry
Soil acidification is a major problem in soils of intensive Chinese agricultural systems. We used two nationwide surveys, paired comparisons in numerous individual sites, and several long-term monitoring-field data sets to evaluate changes in soil acidity. Soil pH declined significantly (P < 0.001) from the 1980s to the 2000s in the major Chinese crop-production areas. Processes related to nitrogen cycling released 20 to 221 kilomoles of hydrogen ion (H+) per hectare per year, and base cations uptake contributed a further 15 to 20 kilomoles of H+ per hectare per year to soil acidification in four widespread cropping systems. In comparison, acid deposition (0.4 to 2.0 kilomoles of H+ per hectare per year) made a small contribution to the acidification of agricultural soils across China.
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