南方红壤侵蚀区土壤肥力质量的突变——以福建省长汀县为例
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1.福建师范大学地理科学学院,350007,福州

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国家自然科学基金(40871141,41001170,41171232)


Mutation of soil fertility quality in the red eroded area of southern China:A case study in Changting County, Fujian Province
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College of Geographical Sciences,Fujian Normal University,College of Geographical Sciences,Fujian Normal University

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    摘要:

    以南方红壤侵蚀区典型区域福建省长汀县为研究区,将土壤肥力质量10个因子作为内部因子,坡度、植被覆盖度、水土流失强度等作为外部因子,构建土壤肥力质量演变的尖点突变模型,并分析土壤肥力质量演变分别与土壤肥力质量等级、水土流失强度、坡度和植被覆盖度的关系。研究结果表明:1)90个样点中,突变的样点共27个,占30%,稳定的样点共63个,占70%;2)突变样点主要对应于土壤肥力质量等级1和等级2(分别占突变样点总数的48.15%和33.33%)、水土流失微度和轻度(分别占37.04%和44.44%)、坡度5-10°和10-15°(分别占37.04%和40.74%)、植被覆盖度>0.4和0.3-0.4(分别占48.15%和37.04%);分叉集Δ与土壤肥力质量等级、水土流失强度、坡度和植被覆盖度都呈极显著(P<0.01)相关关系,皮尔逊相关系数绝对值的大小顺序为:水土流失强度>植被覆盖度>土壤肥力质量等级>坡度;突变主要发生于土壤肥力质量等级较高、水土流失强度较轻、坡度中等、植被覆盖较好的地点;3)土壤肥力质量演变时间相对较长,应根据中间过渡状态来判断是否产生突变;土壤肥力质量处于突变状态时可用较小投入产生较大效益,在关注严重水土流失区生态恢复与重建的同时,不应忽视突变区的治理。

    Abstract:

    This study was conducted in Changting County, Fujian Province, the typical representative area of eroded red soil in Southern China. The internal factors namely ten soil fertility quality factors were selected and the soil fertility quality grade was generated by weighting ten factors based on SPSS. The external factors including soil and water loss intensity, slope and vegetation cover were estimated by 3S technique and field investigation, DEM and TM images, respectively. Mutations were achieved on the base of cusp mutation model constructed by the internal factors and the external factors, and then the relationships between soil fertility quality evolution and soil fertility quality grade, soil and water loss, slope, vegetation coverage were evaluated separately. The following conclusions were drawn from this research: 1) Among 90 soil samples, the numbers of mutational soils and stable soils were 27 and 63 respectively and their proportions took up 30% and 70% respectively. 2) The mutational soils distributed mainly in soil fertility quality grade 1 and 2 (48.15% and 33.33% respectively), very low and low soil and water loss (37.04% and 44.44% respectively), 5-10 degree and 10-15 degree slope (37.04% and 40.74% respectively), vegetation cover >0.4 and 0.3-0.4 (48.15% and 37.04% respectively). There existed very significant correlations(P<0.01)between Δ and soil fertility quality grade, soil and water loss, slope, vegetation cover respectively, and the order of absolute values of Pearson correlation coefficients was soil and water loss > vegetation cover > soil fertility quality grade > slope. Mutation mainly existed in the area where there is high soil fertility quality, low soil and water loss, moderate slope and high vegetation cover. 3) There is a long period during soil fertility quality evolution, and the discrimination of mutation should be based on the stability of intermediate transition. The more benefit would be achieved with less investment when soil fertility quality was mutational, so the treatment of mutational area should not be ignored while ecological restoration and rehabilitation in serious erosion region were took into account.

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陈志强,陈志彪.南方红壤侵蚀区土壤肥力质量的突变——以福建省长汀县为例.生态学报,2013,33(10):3002~3010

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