Spatial Difference of Soil Particle Size Distribution in an Ephemeral Gully Under

YANG Wenli; ZHU Pingzong; CHENG Hong; YAN Jingkun; CHEN Baosheng; YANG Jun

doi:10.13870/j.cnki.stbcxb.2018.04.025

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Spatial Difference of Soil Particle Size Distribution in an Ephemeral Gully Under

更新时间：2025-03-12

- Spatial Difference of Soil Particle Size Distribution in an Ephemeral Gully Under
- Vol. 32, Issue 4, Pages: 158-162(2018)
- 作者机构：
  
  南昌工程学院水利与生态工程学院,南昌,330099
- 作者简介：
- 基金信息：
- DOI：10.13870/j.cnki.stbcxb.2018.04.025
  CLC：
- Published：2018
- 稿件说明：
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YANG Wenli, ZHU Pingzong, CHENG Hong, et al. Spatial Difference of Soil Particle Size Distribution in an Ephemeral Gully Under[J]. 2018, 32(4): 158-162.
DOI：

YANG Wenli, ZHU Pingzong, CHENG Hong, et al. Spatial Difference of Soil Particle Size Distribution in an Ephemeral Gully Under[J]. 2018, 32(4): 158-162. DOI： 10.13870/j.cnki.stbcxb.2018.04.025.

摘要

为研究马尾松林地浅沟侵蚀对地表特征的影响，选取南方红壤区马尾松人工林地发育完整的浅沟为研究对象，采用野外调查与室内试验分析相结合的方法，研究浅沟表层（0—5 cm）土壤颗粒分布的空间差异性。结果表明：（1）研究区内表层土壤颗粒中石砾含量较高，约占78.68%，土壤为多砾质沙土，土壤水蚀使得浅沟表层土壤粗化。（2）浅沟不同部位间表层土壤颗粒分布差异明显，其中石砾含量表现为沟底P<0.01）；极粗砂、中粗砂、细砂粒、粉粒和黏粒含量均表现为沟底 > 沟坡 > 沟缘，且沟底的含量均极显著大于沟坡和沟缘的含量（P<0.01）；而沟坡和沟缘土壤颗粒含量差异不显著（P>0.05）。（3）沿沟长方向从沟头到沟口，沟底表层土壤中粗颗粒含量呈减小趋势，细颗粒含量呈增大趋势；而沟坡和沟缘趋势正好相反，说明在浅沟沟底中上部主要为侵蚀作用，而在中下部主要为沉积作用。（4）不同粒级土壤颗粒含量最优半方差函数理论模型均为高斯模型，土壤颗粒含量的块金系数最大仅为0.36%，远小于25%，不同粒级土壤颗粒含量表现出强烈的空间自相关性。本研究可为南方红壤区人工林地土壤侵蚀治理提供理论支持。

Abstract

A well-developed ephemeral gully

which located in Pinus massoniana forests

was selected as study slope. Then

the spatial distribution characteristics of soil particle size in surface layer (0-5 cm) were studied. The results showed that:(1) The gravel content was higher in topsoil

which texture belonged to sandy. The water erosion led to the coarse soil surface. (2) Soil particle size distributions varied with the different topographic position of ephemeral gully

the content of gravel (>2 mm) showed that the groove P<0.01). All the Extremely coarse sand

coarse sand

fine sand

silt and clay contents were characterized by groove>gully slope>gully edge

and the contents in groove were significantly greater than the gully slope and edge (P<0.01). The difference between soil particle contents in gully slope and edge were not significant (P>0.05). (3) With the gully length direction from head to mizoguchi

the coarse particle contents decreased in groove

but the fine particle contents increased. And the opposite results were found in gully slope and edge. (4) All the optimal semi-variance functions for different graded soil particles were gaussian model

the largest nugget coefficient of soil particles content is only 0.36%

far less than 25%

showing a strong spatial correlation.

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references

吴煜禾,张洪江,程金花,等.重庆四面山不同林地土壤颗粒特征及其与土壤侵蚀的关系[J].水土保持学报,2011,25(5):219-223.

苏里坦,宋郁东,陶辉.不同风沙土壤颗粒的分形特征[J].土壤通报,2008,39(2):244-248.

齐雁冰,常庆瑞,惠泱河.人工植被恢复荒漠化逆转过程中土壤颗粒分形特征[J].土壤学报,2007,44(3):566-570.

张辉,李鹏,鲁克新,等.东柳沟流域表土粒度分布特征及可风蚀性研究[J].水土保持学报,2016,30(5):272-278.

张保华,何毓蓉,徐佩,等.紫色丘陵区小流域侵蚀沉积断面构型及土壤颗粒分形特征[J].水土保持学报,2004,18(6):136-139.

夏江宝,顾祝军,周峰,等.红壤丘陵区不同植被类型土壤颗粒分形与水分物理特征[J].中国水土保持科学,2012,10(5):9-15.

朱丽东,谷喜吉,叶玮,等.洞庭湖周边地区第四纪红土粒度特征及环境意义[J].地理科学进展,2014,33(1):13-22.

毛丽丽,于静洁,张一驰,等.黑河下游土壤的细土颗粒粒径组成和质地类型的空间分布规律初步研究[J].土壤通报,2014,45(1):52-58.

张秦岭,李占斌,徐国策,等.丹江鹦鹉沟小流域不同土地利用类型的粒径特征及土壤颗粒分形维数[J].水土保持学报,2013,27(2):244-249.

茹豪,张建军,李玉婷,等.黄土高原土壤粒径分形特征及其对土壤侵蚀的影响[J].农业机械学报,2015,46(4):176-182.

朱显谟.黄土区土壤侵蚀的分类[J].土壤学报,1956(2):99-115.

陈永宗,景可,蔡强国,等.杏子河流域的侵蚀地貌[J].水土保持通报,1984(5):6-9.

赵其国,黄国勤,马艳芹.中国南方红壤生态系统面临的问题及对策[J].生态学报,2013,33(24):7615-7622.

汪邦稳,段剑,王凌云,等.红壤侵蚀区马尾松林下植被特征与土壤侵蚀的关系[J].中国水土保持科学,2014,12(5):9-16.

郭明明,王文龙,李建明,等.黄土区坡耕地耕作对浅沟径流产沙及其形态发育特征的影响[J].农业工程学报,2015,31(15):114-123.

王冬冬,高磊,陈效民,等.红壤丘陵区坡地土壤颗粒组成的空间分布特征研究[J].土壤,2016,48(2):361-367.

陈晓燕,牛青霞,周继,等.人工模拟降雨条件下紫色土陡坡地土壤颗粒分布空间变异特征[J].水土保持学报,2010,24(5):163-168.

吴淑芳,吴普特,宋维秀,等.黄土坡面径流剥离土壤的水动力过程研究[J].土壤学报,2010,47(2):223-228.

吴冰,邵明安,毛天旭,等.模拟降雨下坡度对含砾石土壤径流和产沙过程的影响[J].水土保持研究,2010,17(5):54-58.

王晓燕,尹洁.坡面小区土壤流失过程中粒径组成变化及其影响因素[J].水土保持学报,2010,24(4):113-118.

胡广录,樊立娟,王德金,等.荒漠-绿洲过渡带斑块植被表层土壤颗粒的空间异质性[J].兰州交通大学学报,2013,32(6):159-164.

张正偲,董治宝.土壤风蚀对表层土壤粒度特征的影响[J].干旱区资源与环境,2012,26(12):86-89.

林正雨,高雪松,邓良基,等.微地形土壤颗粒分形维数的空间变异特征研究[J].土壤通报,2009,40(3):471-475.

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