中国农业科学 ›› 2006, Vol. 39 ›› Issue (9): 1828-1835 .

• 土壤肥料·节水灌溉 • 上一篇    

岩溶峰丛洼地土壤养分空间分异特征及影响因子分析

张伟 陈洪松 王克林 苏以荣 张继光 易爱军   

  1. 中科院亚热带农业生态研究所 中科院亚热带农业生态研究所 中国科学院亚热带区域农业研究所
  • 收稿日期:2006-01-17 修回日期:1900-01-01 出版日期:2006-09-10 发布日期:2006-09-10
  • 通讯作者: 陈洪松

The Heterogeneity of soil nutrients and their influencing factors in peak-cluster depression areas of karst region

  

  1. 中科院亚热带农业生态研究所 中科院亚热带农业生态研究所 中国科学院亚热带区域农业研究所
  • Received:2006-01-17 Revised:1900-01-01 Online:2006-09-10 Published:2006-09-10

摘要: 研究了典型岩溶峰丛洼地土壤养分在坡地和洼地的空间分异特征,并探讨了土地利用方式和地形因子对土壤养分空间分布的影响。结果表明:土壤养分在坡地和洼地存在显著差异,受长期耕作影响,有机碳、全氮、全磷、全钾、碱解氮和速效钾在洼地的含量显著低于坡地。而速效磷在洼地的含量显著高于坡地,说明施肥对土壤的有效磷含量具有重要作用;在坡面尺度,土地利用方式是有机碳、全氮、全磷、全钾、碱解氮、速效磷等养分的主要影响因子。地形因子对有机碳等上述养分和速效钾、PH值有显著影响,但其方差贡献均小于土地利用方式(速效钾和PH值除外);种植制度对洼地土壤有机碳、全磷、全钾、速效钾有显著影响,牧草地在一定程度上有利于有机质的积累;有机碳、全氮、碱解氮等养分整体表现为随着土地利用强度的增加而显著降低,自然坡地和撂荒地的有机碳含量较高,分别为耕地的3.35倍和1.91倍,生态系统表现为“碳汇”趋势。耕地的有机碳含量显著偏低,生态系统表现为“碳源”趋势,不利于农业生态系统的健康发展。木豆-板栗地的有机碳、全氮等养分显著高于耕地,退耕在一定程度上有利于有机质等养分的积累,但是对坡面尺度土壤养分的分析表明木豆-板栗地的有机碳等养分显著低于自然坡地和撂荒地,说明土壤理化性质要恢复到自然水平,还需要较长时间。

关键词: 岩溶峰从洼地, 土壤养分, 土地利用方式, 地形因子, 土壤有机碳

Abstract: Selecting a typical karst peak cluster-depression system in northwest Guangxi Autonomous region, we have evaluated the effects of land-uses and topographic factors on soil nutrients. The results indicated that: with a long-term of tillage, soil organic carbon (SOC), total nitrogen (TN), total phosphorus (TP), total potassium (TK), available nitrogen (AN) and available potassium (AK) in depression are significantly lower than slope land. Yet the available phosphorus (AP) is significantly higher than that of slope land,and it may be implied that fertilizer input was very important for AP in soil; SOC, TN, TP, TK, AN and AP were highly affected by Land-uses in slope-line scale. Topographic factors have a significant effect on SOC, TN, TP, AN, AP, AK and PH, but its variance ratio is lesser than land-use type; In the depression, different cropping systems have a significant effect on SOC, TP, TK and AK, though its variance ratio is low, it reflected the difference of fertilization and crop character among cropping systems; In research area, SOC, TN and AN decrease significantly with land-use intensity increases. Nature field and abandoned field have a higher accumulation of SOC, and it’s SOC contents is 3.35 times and 1.91 times of the tillage field. As a result of erosion and leaching, witch are induced by cultivation (or past cultivation), tillage field have a lower accumulation of SOC, TN and AN. SOC, TN, TK, AN and AK is significantly higher in rehabilitated field than in tillage field on research area scale, converting cropland to forest-land has a positive effect on soil organic matter accumulation. But on slope-line scale, SOC, TN, TP, AN and AK in rehabilitated field is significantly lower than in Nature field and abandoned field, suggesting that physical and chemical property changes within the degradation soil may take a longer periods to the nature level.

Key words: karst peak-cluster depression, soil nutrient, land-use type, topography indices, soil organic carbon