|Table of Contents|

Spatial and Temporal Variability of Soil Moisture and Bulk Density of Abandoned Land in Loess Hilly Region of Northern Shaanxi(PDF)

《北方园艺》[ISSN:1001-0009/CN:23-1247/S]

Issue:
2013年13期
Page:
192-197
Research Field:
Publishing date:

Info

Title:
Spatial and Temporal Variability of Soil Moisture and Bulk Density of Abandoned Land in Loess Hilly Region of Northern Shaanxi
Author(s):
HAO Wen-fang1DU Feng2CHEN Cun-gen3LIANG Zong-suo12
1.College of Life Science,Northwest Agricultural and Forestry University,Yangling,Shaanxi 712100;2.Institute of Soil and Water Conservation,Chinese Academy of Science and Ministry of Water Resources,Yangling,Shaanxi 712100;
3.College of Forestry,Northwest Agricultural and Forestry University,Yangling,Shaanxi 712100
Keywords:
loess hilly region of Northern Shaanxiabandoned landsoil moisturesoil bulk densityspatial and temporal variability
PACS:
S 152
DOI:
-
Abstract:
With 30 abandoned lands in hilly area in region of Northern Shaanxi as experiment object,during their natural recovery process,spatial sequence generation of timeseries were used,the monthly and yearly alteration of their soil moisture and the temporal variability of their soil bulk was analyzed.The results showed that the abandoned arable land made the soil bulk density become smaller;in the vertical profile,soil moisture increased with the increase of the soil depth;the changing tendency of soil moisture of abandoned arable land was shady>semi shady>semi sunny slope>sunny;monthly changing tendency of soil moisture of abandoned arable land was July>August>September>October>May>June;the inter annual dynamics of soil water content was that soil moisture of 2005 was higher than that of 2006 and 2007.In the three years from 2005 to 2007,the soil moisture was higher in the early succession stage,then decreased.

References:

[1]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.

[2]郑华,欧阳志云,王效科.不同森林恢复类型对南方红壤侵蚀区土壤质量的影响[J].生态学报,2004,24(9):1994-2002.
[3]郝文芳.陕北黄土丘陵区撂荒地恢复演替的生态学过程及机理研究[D].杨凌:西北农林科技大学,2010.
[4]廖善刚,叶志君,汪严明.桉树人工林与杉木林、毛竹林土壤理化性质对比研究[J].亚热带资源与环境学报,2008(3):54-55.
[5]黄宇,汪思龙,冯宗炜.不同人工林生态系统林地土壤质量评价[J].应用生态学报,2004,15(12):2199-2205.
[6]南京大学.土壤农化分析[M].北京:农业出版社,1986.
[7]郝文芳,韩蕊莲,单长卷,等.黄土高原不同立地条件下人工刺槐林土壤水分变化规律研究[J].西北植物学报,2002,23(6):964-968.
[8]韩仕峰,李玉山,张孝忠,等.黄土高原地区土壤水分区域动态特征[J].中国科学院西北水土保持研究所集刊,1989(10):161-167.
[9]胡梦郡,刘文兆,赵姚阳.黄土高原农、林、草地水量平衡异同比较分析[J].干旱地区农业研究,2003,21(4):113-116.
[10]马玉玺,杨文治,杨新民.陕北黄土丘陵沟壑区刺槐林水分生态条件及生产力研究[J].水土保持通报,1999,10(6):7475.[11]杜峰,山仑,梁宗锁,等.陕北黄土丘陵区撂荒演替过程中的土壤水分效应[J].自然资源学报,2005,20(5):669-678.
[12]庞敏,侯庆春,薛智德,等.延安研究区主要自然植被类型土壤水分特征初探[J].水土保持学报,2005,19(2):138-141.
[13]徐学选,张北赢,白晓华.黄土丘陵区土壤水资源与土地利用的耦合研究[J].水土保持学报,2007,21(3):166-169.
[14]焦峰,温仲明,焦菊英,等.黄丘区退耕地植被与土壤水分养分的互动效应[J].草业学报,2006,15(2):79-84.
[15]Sala O E,Golluscio R A,Lauenroth W K,et al.Resource partitioning between ?shrubs and grasses in the Patagonian steppe[J].Oecologia,1989,81:501-505.
[16]张庆费,宋永昌.浙江天童植物群落次生演替与土壤肥力的关系[J].生态学报,1999,19(2):174-17.
[17]郝文芳,梁宗锁,陈存根,等.黄土丘陵区弃耕地群落演替过程中的物种多样性研究[J].草业科学,2005(9):1-7.

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Last Update: 2014-08-08