[1]ZHANG Jun-bin,HUANG Yong-Jie,LIANG Da-qing.Study on the Distributions Change of Soil and Water Properties under Different Slope Land[J].Research of Soil and Water Conservation,2007,14(01):301-304.
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Study on the Distributions Change of Soil and Water Properties under Different Slope Land

References:
[1] 朱继鹏,王芳,高甲荣.吉县蔡家川流域不同森林植被的林地水源涵养功能[J].水土保持研究2006,13(4):111-114.
[2] 张仲民.土壤化育与形态学[M]."国立编译馆",1981.
[3] Lyle Prunty and Joel Bell.Soil Temperature Change over Time during Infiltration[J].Soil Sci.Soc.Am.J,2005,69:766-775.
[4] 林俐玲,蔡义志,杜怡德.陡坡茶园水土流失机制之研究[J]."水土保持学报",2001,33(1):15-24.
[5] 王政权.地理统计学及在生态学中的应用[M].科学出版社,1999.
[6] 夏禹九,金恒镳,洪富文,等.植生型与施肥作业对滨岸带土壤水化学性质的影响[J].林业试验所研究报告季刊,1994,9(1):39-50.
[7] 王效举.红壤丘陵区不同土地利用方式下土壤变化特征的研究[J].资源科学,1998,20(5):24-31.
[8] 李家永,袁小华.红壤丘陵区不同土地资源利用方式下有机碳储量的比较研究[J].资源科学,2001,23(5):73-76.
[9] 马海艳,龚家栋,王根绪,等.干旱区不同荒漠植被土壤水分的时空变化特征分析[J].水土保持研究,2005,12(6):231-234.
[10] 钱亦兵,周华荣,赵锐锋,等.塔里木河中下游湿地及其外围土壤性质性状的空间异质性[J].水土保持学报,2005,19(6):31-34.
[11] 石培礼,于贵瑞.拉萨河下游河谷不同土地利用方式下土壤有机碳储量格局[J].资源科学,2003,25(5):96-102.
[12] 李土生,姜志林.苏南丘陵主要森林类型保持水土效益的研究[J].长江流域资源与环境,1994,3(1):55-59.
[13] 陆象豫.森林在水土资源保育上之功能[J].台湾林业科学,1996,11(3):333-347.
[14] 钟慕龙,黄树才,杨民胜,等.不同林龄桉树人工林森林空间结构差异研究[J].广东林业科技,2005,21(4):1-4.
[15] Folliott,P F,W P Clary,J R Davis.Some characteristics of the forest floor under ponderosapine in Arizona[M].U.S.Forest Service Research Note RM-27,1968.
[16] 孙丞虎,利瓦伊京,张祖强,等.淮河流域土壤湿度异常的时空分布特征及其与气候异常关系的初步研究[J].应用气象学报,2005,16(2):129-138.
[17] Adu,J K,J M Oades.Physical factors influencing decomposition of organic materials in soil aggregates[J].Soil Biology and Biochemistry,1978,10:109-115.
[18] 卢惠生,林壮沛,黄良鑫.莲华池地区天然阔叶林不同土壤深度的温度日周期变化[J].中华水土保持学报,2000,31(4):267-278.
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