Physical Properties of Soils Developed from Different Parent Rocks in Yimeng Mountainous Region

ZHANG Yong-kun; WU Yuan-zhi; YU Xing-xiu

doi:10.13961/j.cnki.stbctb.2014.05.014

您当前的位置：

首页 >

文章列表页 >

Physical Properties of Soils Developed from Different Parent Rocks in Yimeng Mountainous Region

- Physical Properties of Soils Developed from Different Parent Rocks in Yimeng Mountainous Region
- Bulletin of Soiland Water Conservation Vol. 33, Issue 5, Pages: 34-38(2014)
- 作者机构：
  
  1. 临沂大学水土保持与环境保育研究所山东省水土保持与环境保育重点实验室,山东,临沂,276000
  2. 山东师范大学人口&#,183
  3. 资源与环境学院,山东,济南,250014
  4. 湖北大学资源环境学院,湖北,武汉,430000
- 作者简介：
- 基金信息：
- DOI：10.13961/j.cnki.stbctb.2014.05.014
  CLC：
- Published：2014
- 稿件说明：
移动端阅览
ZHANG Yong-kun, WU Yuan-zhi, YU Xing-xiu. Physical Properties of Soils Developed from Different Parent Rocks in Yimeng Mountainous Region[J]. Bulletin of Soiland Water Conservation, 2014, 33(5): 34-38.
DOI：

ZHANG Yong-kun, WU Yuan-zhi, YU Xing-xiu. Physical Properties of Soils Developed from Different Parent Rocks in Yimeng Mountainous Region[J]. Bulletin of Soiland Water Conservation, 2014, 33(5): 34-38. DOI： 10.13961/j.cnki.stbctb.2014.05.014.

摘要

以沂蒙山区小圣堂小流域为研究区

对比分析了酸性岩石和钙质岩石发育土壤的物理性质及其影响因素。结果表明:(1)酸性岩石发育土壤石砾及砂粒含量较高

土壤质地由砂壤质到壤砂质

且随土层深度增加

石砾含量增加。钙质岩石发育土壤粉粒及黏粒含量较高

上下两层的土壤颗粒组成相差不大。受成土母岩影响两种土壤分形维数都很低

且酸性岩石发育土壤的分形维数更低。两种土壤石砾含量均大于10%

为粗骨土。(2)酸性岩石发育土壤的容重较大

总孔隙度和毛管孔隙度较小。两种土壤的容重和毛管孔隙度随土层深度的增加而变大

总孔隙度和非毛管孔隙度则反之。毛管孔隙度大小主要受土壤分形维数的影响。(3)酸性岩石发育土壤的饱和导水率大于钙质岩石发育土壤

酸性岩石发育土壤10-20 cm土层的饱和导水率较0-10 cm土层大

而钙质岩石发育土壤饱和导水率在不同土层深度呈现不规律的变化。土壤质地是影响沂蒙山区土壤饱和导水率的主导因素

其中

砂粒和粉粒含量的影响尤为明显。

Abstract

A comparative analysis of soil physical properties and their influencing factors was carried out between soils developed from either acidic and calcareous rocks in Xiaoshengtang small watershed in the Yimeng mountainous region. The results showed that:(1) The soils developed from acidic rocks contained more gravel and sand than those from calcareous rocks. Soil textures ranged from sandy loam to loamy sand

and the gravel content increased with soil depth. The silt and clay contents of the soils were slightly higher in soils developed from calcareous rocks than from acidic rocks. However

the particle size compositions of the upper and lower soil layers were similar for soils from the calcareous rocks. Both soil types had relatively low fractal dimensions

which were influenced by the parent rock

but those of the soils developed from acidic rock were lower. Furthermore

they were both poorly developed soils with gravel contents higher than 10%.(2) Soils developed from acidic rock had higher bulk densities than that from calcareous rocks

which had higher total and capillary porosities. The bulk densities and capillary porosities of the two soils increased with increasing soil depth and

conversely

the total porosities and non-capillary porosities decreased. Furthermore

the capillary porosities were mainly influenced by soil fractal dimensions.(3) The saturated hydraulic conductivities of the soils developed from acidic rock were higher than those from calcareous rock

and they were higher in the 10-20 cm soil layer than in the 0-10 cm layer. However

the saturated hydraulic conductivities of the soils developed from calcareous rock did not exhibit consistent changes in different soil layers. Soil texture

especially the sand and silt contents

was the main influencing factor of soil saturated hydraulic conductivity in the Yimeng mountainous region.

关键词

Keywords

references

Olowolafe E A. Soil parent materials and soil properties in two separate catchment areas on the Jos Plateau, Nigeria[J]. GeoJournal, 2002,56(3):201-212.

Kooijman A M, Jongejans J, Sevink J. Parent material effects on Mediterranean woodland ecosystems in NE Spain[J]. Catena, 2005,59(1):55-68.

Arshad M A, Lowery B, Grossman B. Physical tests for monitoring soil quality Doran J W, Jones A J. Methods for Assessing Soil Quality[M]//Soil Science Society of America Publication, Madison, Wisconsin, USA, 1996:123-141.

Boix-Fayos C, Calvo-Cases A, Imeson A C, et al. Influence of soil properties on the aggregation of some Mediterranean soils and the use of aggregate size and stability as land degradation indicators[J]. Catena, 2001,44(5):47-67.

Karlen D L, Stott D E. A frame work for evaluating physical and chemical indicators of soil qualit[M]//Dorman J W, Coleman D F, Bezdicek F. et al. Defining Soil Quality for a Sustainable Environment Soil Science Society of American Publication, No 35. Madison, Wisconsin, USA, 1994:53-72.

董玲玲,何腾兵,刘元生,等.喀斯特山区不同母质(岩)发育的土壤主要理化性质差异性分析[J].土壤通报,2008,39(3):471-474.

骆东奇,侯春霞,魏朝富,等.不同母质发育紫色土团粒结构的分形特征研究[J].水土保持学报,2003,17(1):131-133,182.

李成亮,何园球,熊又升,等.四种不同母质发育的红壤水分状况研究[J].土壤,2004,36(3):310-317.

依艳丽,冯永军,刘孝义.棕壤和褐土的持水性和供水能力[J].土壤,1995,27(6):290-294.

马履一,翟明普,王勇.京西山地棕壤和淋溶褐土饱和导水率的分析[J].林业科学,1999,35(3):109-112.

山东省土壤肥料工作站.山东省山地丘陵区土壤[M].济南:山东科学技术出版社,1986:38-39.

贾晓红,李新荣,李元寿.干旱沙区植被恢复过程中土壤颗粒分形特征[J].地理研究,2007,26(3):520-524.

邵明安,王全九,黄明斌.土壤物理学[M].北京:高等教育出版社,2006:19-23.

李德成,张桃林.中国土壤颗粒组成的分形特征研究[J].土壤与环境,2000,9(4):263-265.

黄冠华,詹卫华.土壤颗粒的分形特征及其应用[J].土壤学报,2002,39(4):490-497.

党亚爱,李世清,王国栋,等.黄土高原典型土壤剖面土壤颗粒组成分形特征[J].农业工程学报,2009,25(9):74-78.

伏耀龙,张兴昌,王金贵.岷江上游干旱河谷土壤粒径分布分形维数特征[J].农业工程学报,2012,28(5):120-125.

程先富,史学正,王洪杰.红壤丘陵区耕层土壤颗粒的分形特征[J].地理科学,2003,23(5):617-621.

杨弘,李忠,裴铁璠,等.长白山北坡阔叶红松林和暗针叶林的土壤水分物理性质[J].应用生态学报,2007,18(2):272-276.

Putuhena W M, Cordery I. Estimation of interception capacity of the forest floor[J]. Journal Hydrology, 1996,180(1):283-299.

叶仲节,柴锡周.浙江林业土壤[M].杭州:浙江科学技术出版社,1986:77-103.

田大伦, 陈书军. 樟树人工林土壤水分-物理性质特征分析[J].中南林学院学报,2005,34(2):1-6.

杨建,陈家军,杨周喜,等.松散砂粒孔隙结构、孔隙分形特征及渗透率研究[J].水文地质工程地质,2008,35(3):93-98.

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):1896-1896.

郑纪勇,邵明安,张兴昌.黄土区坡面表层土壤容重和饱和导水率空间变异特征[J].水土保持学报,2004,18(3):53-56.

王贤,张洪江,程金花,等.重庆市四面山典型林分土壤饱和导水率研究[J].水土保持通报,2012,32(2):29-34.

丁小龙,张兴昌,窦晶晶,等.EN-1固化剂对4种土壤饱和导水率的影响研究[J].水土保持通报,2012,32(1):132-134.

贾小旭,邵明安,魏孝荣,等.黄土高原北部草地表层土壤水分状态空间模拟[J].农业工程学报,2010,26(10):38-44.

Views

1697

下载量

CSCD

Alert me when the article has been cited

提交

Tools

Publicity Resources

Changes of Infiltration Characteristics of Abandoned Cropland with Plant Restoration in Loess Hilly Region

Change of Soil Physical Properties with Precipitation Gradient in Desert Region of Hexi Corridor

Effects of EN-1 Solidifying Agent on Saturated Hydraulic Conductivity of Four Soils

Physical Characteristics of Soil Moisture and Their Altitude Effects for Different Forest Stand Types in Fengyang Mountains of Zhejiang Province

Structure and variation characteristics of agricultural non-point source pollution in Qinghai Province from 2009 to 2023

Related Author

WANG Guo-liang

LIU Guo-bin

BO Hai-feng

WU Li-yu

ZHAO Wen-zhi

WANG Hui

HU Hong-chang

LI Chun-jie

Related Institution

Institute of Soil and Water Conservation, Chinese Academy of Sciences and Ministry of Water Resources, Yangling

Northwest Sci-Tech University of Agriculture & Forestory,Yangling

Linze Inland River Basin Research Station, Laboratory of Basin Hydrology and Ecology, Cold and Arid RegionsEnvironmental and Engineering Research Institute, Chinese Academy of Sciences

College of Forestry, Gansu Agricultural University

Institute of Mountain Hazards and Environment,CAS

⁰