Acidity Characteristics and Influencing Factors of Tobacco-planting Soils in Wuling Mountains——A Case Study in Xiangxi Autonomous Prefecture, Hunan Province
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Acidity Characteristics and Influencing Factors of Tobacco-planting Soils in Wuling Mountains——A Case Study in Xiangxi Autonomous Prefecture, Hunan Province
DENG Xiaohua, LI Yuanhuan, ZHOU Miliang, et al. Acidity Characteristics and Influencing Factors of Tobacco-planting Soils in Wuling Mountains——A Case Study in Xiangxi Autonomous Prefecture, Hunan Province[J]. 2018, 32(4): 304-309.
DOI:
DENG Xiaohua, LI Yuanhuan, ZHOU Miliang, et al. Acidity Characteristics and Influencing Factors of Tobacco-planting Soils in Wuling Mountains——A Case Study in Xiangxi Autonomous Prefecture, Hunan Province[J]. 2018, 32(4): 304-309. DOI: 10.13870/j.cnki.stbcxb.2018.04.048.
Acidity Characteristics and Influencing Factors of Tobacco-planting Soils in Wuling Mountains——A Case Study in Xiangxi Autonomous Prefecture, Hunan Province
In order to comprehend the acidity characteristics of mountainous soils planted tobacco for many years
the characteristics of soil acidity index and their relations were studied in Xiangxi Autonomous Prefecture
as well as the effects of planting years
soil types
organic matter and clay on soil acidity were studied. The results were as follows:(1) The effect of tobacco planting years on soil acidity in Wuling mountain area was greater than that of soil types
and with the increasing of planting years
the soil pH
the exchangeable base cations
cation exchange capacity and base saturation of yellow-brown soil decreased
while the potential acidity increased. (2) The relationship between soil pH and exchangeable acid was a power function
and exchangeable Alex was the main body of exchangeable acid in soil
the strength of soil exchangeable acid increased with the increasing of exchangeable Alex and its relative proportion. (3) The relationship between soil pH and exchangeable base cations
cation exchange capacity and base saturation was a quadratic curve
and when the soil pH was less than 6
the exchangeable base cations and cation exchange capacity decreased with the increasing of soil pH
while the base saturation increased; when soil pH was more than 6
the exchangeable base cations and cation exchange capacity increased with the increasing of soil pH
while base saturation fluctuated slightly. (4) Soil exchangeable base ions were mainly exchangeable calcium
followed by exchangeable magnesium
and the exchangeable calcium was the most important factor influenced soil pH. (5) Soil organic matter and clay mainly affected the soil pH
cation exchange capacity
exchangeable base cations and exchangeable calcium.
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