1. 中国科学院亚热带农业生态研究所亚热带农业生态过程重点实验室,湖南,长沙,410125
2. 中国科学院环江喀斯特生态系统观测研究站, 广西环江,547100
纸质出版:2010
移动端阅览
陈洪松, 侯娅, 张伟, 等. 桂西北典型环境移民迁入区土壤养分特征分析[J]. 水土保持通报, 2010,29(4):6-10.
CHEN Hongsong, HOU Ya, ZHANG Wei, et al. Soil Nutrient Characteristics in Typical Immigrant Region of Northwest Guangxi Province[J]. Bulletin of Soiland Water Conservation, 2010, 29(4): 6-10.
在桂西北典型环境移民迁入区
分析了5种土地利用方式表层(0—20cm)土壤有机质(SOM)、全量养分和速效养分的变化特征。结果表明
根据变异系数(CV)大小
除速效磷(AP)为强变异外(CV>1.0)
其余土壤养分都为中等变异(0.1<CV<1.0)。整体而言
移民迁入区SOM、全氮(TN)含量处于较高水平
速效氮(AN)、速效磷(AP)含量处于中等水平
全磷(TP)、速效钾(AK)处于偏低水平
而全钾(TK)处于低水平。土地利用方式是影响土壤养分的主要因素。灌丛和荒草地的SOM
TN
AN处于较高水平
果园和旱地则处于中等水平;次生林SOM处于较高水平
TN处于中等水平
而AN处于偏低水平。除旱地和果园AP含量处于中等水平外
不同利用方式土壤的TP
TK
AP
AK含量处于低或偏低水平。由于采取了较好的水土保持措施
移民后较大规模的土地利用变化没有导致明显的土壤退化
但需要增加磷钾肥的施用量。
Five typicalland use types were chosen in the representative environmental immigrant region of Northwest Guangxi
China. Soil organic matter (SOM) and total and available nutrient contents were analyzed in the surface soil layer (0) 20cm). Results showed that in terms of the coefficient of the variation (CV) of soil nutrients
the contents of SOM
total N(TN)
total P(TP)
total K(TK)
available N(AN)
and available K(AK) had a moderate variability(0.1V1.0)
except that available P(AP) content had a high variability(CV1.0). In general
SOM and TN contents were in a higher level
AN and AP contents were in a moderate level
TP and AK contents were in a low level
and TK content was in a lower level.Land use had an important effect on the change in soil nut rients. SOM
TN
and AN contents had a high level in shrubland and grassland and a moderate level in dry land and or char dland. SOM
TN
and AN co ntents had a high
moderate
and low levels in seco ndary forest land
respectively. TP
TK
A P
and AK contents had low and lower levels in five land use types except that AP had a moderate level in dry land and orchar dland. Land use change after immigration did not lead to obv io us soil deg radat ion due to effective soil and water conserv ation measures
but P and K nutrients were increased.
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