[1]JIANG Fang-shi,HUANG Yan-he,LIN Jin-shi,et al.Soil Particle Size Distribution and Fractal Dimensions of Colluvial Deposits in Granite Benggang[J].Research of Soil and Water Conservation,2014,21(06):175-180.
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Soil Particle Size Distribution and Fractal Dimensions of Colluvial Deposits in Granite Benggang
Research of Soil and Water Conservation[ISSN 1005-3409/CN 61-1272/P] Volume:
21
Number of periods:
2014 06
Page number:
175-180
Column:
Public date:
2014-12-28
- Title:
- Soil Particle Size Distribution and Fractal Dimensions of Colluvial Deposits in Granite Benggang
- CLC:
- S152.3
- DOI:
- -
- Abstract:
- Colluvial deposit, as a part of hill, has high contents of loose materials and high erodibility, and the particle composition and the fractal dimensions of colluvial soil have its own characteristics. Soil particle size distribution of colluvial deposits and clasping wall in granite hill were analyzed by using the laser article size distribution instrument. The results indicated that colluvial deposits were given priority with gravel, sand and silt contents, clay content was extremely low, the gravel soil was the dominated soil texture; the average fractal dimensions of soil particles of colluvial deposits were less than the range between 2.61 to 2.70, which reflected the characteristic of fine particle loss; clay content was the major factor of the fractal dimension; the fractal dimension could reflect the soil physical and chemical properties of collapsing wall, but it couldn’t reflect the soil properties of colluvial deposits.
- References:
-
[1] 唐克丽.中国水土保持[M].北京:科学出版社,2004.
[2] 蒋芳市,黄炎和,林金石,等.崩岗崩积体土壤渗透特性分析[J].水土保持学报,2013,27(3):49-54.
[3] 何腾兵.贵州山区土壤物理性质对土壤侵蚀影响的研究[J].土壤侵蚀与水土保持学报,1995,1(1):85-95.
[4] 陈子玉,顾祝军.南方水蚀区不同侵蚀程度土壤粒径分形研究[J].水土保持研究,2013,20(4):13-16.
[5] 吴尧,姚健,吴永波,等.岷江上游典型植被下土壤分形特征及对水分入渗的影响[J].水土保持通报,2012,32(2):12-16.
[6] 罗明达,杨吉华,房用,等.沂源石灰岩山地不同植被类型土壤颗粒分形特征研究[J].水土保持研究,2010,17(3):17-21.
[7] 吴志峰.华南花岗岩风化土体粒度成分的分形特征[J].中国水土保持,1997(5):17-19.
[8] 高君亮,李玉宝,虞毅,等.毛乌素沙地不同土地利用类型土壤分形特征[J].水土保持研究,2010,17(6):220-223.
[9] 朱华,程先富,王世航,等.基于GIS的安徽省表层土壤颗粒分形特征研究[J].水土保持研究,2009,16(4):146-149.
[10] 林敬兰,黄炎和.崩岗侵蚀的成因机理研究与问题[J].水土保持研究,2010,17(2):41-44.
[11] 林敬兰,黄炎和,蒋芳市,等.崩岗土体的渗透性能机理研究[J].水土保持学报,2013,27(2):53-56.
[12] 鲁如坤.土壤农业化学分析方法[M].北京:中国农业科技出版社,2000.
[13] 中国科学院南京土壤研究所土壤物理研究室.土壤物理性质测定法[M].北京:科学出版社,1978.
[14] 刘目兴,聂艳,于婧.不同初始含水率下粘质土壤的入渗过程[J].生态学报,2012,32(3):871-878.
[15] 杨培岭,罗远培,石元春.用粒径的重量分布表征的土壤分形特征[J].科学通报,1993,38(20):1896-1899.
[16] 郭中领,符素华,王向亮,等.北京地区表层土壤分形特征研究[J].水土保持通报,2010,30(2):154-158.
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