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[1]PAN Zhan-bing,ZHANG Long,YANG Rui,et al.Overview on Research Progress of Soil Drought in Semiarid Regions of the Loess Plateau[J].Research of Soil and Water Conservation,2012,19(06):287-291,298.

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Overview on Research Progress of Soil Drought in Semiarid Regions of the Loess Plateau

Research of Soil and Water Conservation[ISSN 1005-3409/CN 61-1272/P] Volume: 19 Number of periods: 2012 06 Page number: 287-291,298 Column: Public date: 2012-12-20

Title:: Overview on Research Progress of Soil Drought in Semiarid Regions of the Loess Plateau

Author(s):: PAN Zhan-bing¹, ZHANG Long^1,2, YANG Rui³, LI Sheng-bao¹, DONG Li-guo¹, CAI Jin-jun¹; 1. Ningxia Academy of Agriculture and Forestry Sciences, Yinchuan 750002, China;
2. School of Agriculture, Ningxia University, Yinchuan 750021, China;
3. Yongning Center for Agricultural Technology Extension and Service, Yongning, Ningxia 750100, China

Keywords:: semiarid regions; soil drought; quantitative evaluation; mitigation measure

CLC:: S152.7

DOI:: -

Abstract:: As the result of scarce precipitation, excessive water consumption by vegetation and quick evaporation in semi-arid area, the soil is so dry in a long term that the dry layers formed in the profile. It is difficult to be wetted soon once the dry earth layers occurred, which will cause serious influence on the development of ecological environment and economy. The causes of soil dry layer was analyzed and it’s definition was given. The method of quantitative evaluation and reducing drought is also explained. The defect of the soil desiccation quantitative research nowadays was showed. It was suggested that the future research should focus on the research of soil drought evaluation index affecting plant growth, and pay more attention to research for vegetation construction based on soil water security in order to avoid accelerating soil drought caused by human.

References:: [1] 杨文治,邵明安,彭新德,等.黄土高原环境的旱化与黄土中水分关系[J].中国科学,1998,28(4):357-365.
[2] 西北水土保持与生物研究组.陕西省东都干旱农地土壤水分调查[J].土壤,1975,28(6):279-285.
[3] 侯庆春,韩蕊莲,韩仕峰.黄土高原人工林草地"土壤干层"问题初探[J].中国水土保持,1999(5):11-14.
[4] 李玉山.苜蓿生产力动态及其水分生态环境效应[J].土壤学报,2002,39(3):404-411.
[5] 朱香凝,郭继勋,梁存柱,等.华北平原地区灌溉对苜蓿产量及土壤水分的影响[J].中国草地,2002,24(6):32-37.
[6] 王美艳,李军,孙剑,等.黄土高原半干旱区苜蓿草地土壤干燥化特征与粮草轮作土壤水分恢复效应[J].生态学报,2009,29(8):4528-4534.
[7] 李玉山.黄土高原森林植被对陆地水循环影响的研究[J].自然资源学报,2001,16(5):427-432.
[8] 杨文治,余存祖.黄土高原区域治理与评价[M].北京:科学出版社,1992.
[9] 王力,邵明安,侯庆春.延安试区土壤干层现状分析[J].水土保持通报,2000,20(3):35-37.
[10] 程积民,万惠娥,王静,等.半干旱区柠条生长与土壤水分消耗过程研究[J].林业学报,2005,41(2):37-41.
[11] 程积民,万惠娥,王静.黄土丘陵区苜蓿生长与土壤水分变化[J].应用生态学报,2005,16(3):435-38.
[12] 肖军,赵景波.黄土高原地区土壤干层综合研究[J].固原师专学报:自然科学版,2005,26(6):58-61.
[13] 赵景波.淀积理论与黄土高原环境演变[M].北京:科学出版社,2002.
[14] 李裕元,邵明安.黄土高原气候变迁、植被演替与土壤干层的形成[J].干旱区资源与环境,2001,5(1):2-77.
[15] 杜娟,赵景波.长安少陵塬全新世以来的土壤侵蚀规律研究[J].中国沙漠,2004,24(1):63-70.
[16] 张海,王延平,高鹏程,等.黄土高原坡地土壤干层形成机理及补水途径研究[J].水土保持学报,2003,17(3):162-164.
[17] 杜世平,王留芳,龙明秀.宁南山区旱地紫花苜蓿土壤水分及产量动态研究[J].草业科学,1999,16(1):12-17.
[18] 刘刚,王志强,王晓岚.吴旗县不同植被类型土壤干层特征分析[J].水土保持研究,2004,11(1):126-129.
[19] 李军,陈兵,李小芳,等.黄土高原不同干旱类型区苜蓿草地深层土壤干燥化效应[J].生态学报,2007,27(1):75-89.
[20] 王俊,刘文兆,李风民.半干旱区不同作物与苜蓿轮作对土壤水分恢复与肥力消耗的影响[J].土壤学报,2004,44(1):179-183.
[21] 王力,邵明安,侯庆春.土壤干层量化指标初探[J].水土保持学报,2000,14(4):87-90
[22] 刘沛松.宁南旱区苜蓿草地土壤水分消耗规律及粮草轮作土壤水分恢复效应研究[J].土壤肥料科学,2005,21(9):270-274.
[23] Saeed I A M, EI-Nadi A H. Irrigation effects on the growth, yield, and water use efficiency of alfalfa[J]. Irrigation Science,1997,17(2):63-68.
[24] 王力,邵明安,王全九,等.黄土区土壤干化研究进展.农业工程学报,2004,20(5):27-31.
[25] 潘占兵,余峰,王占军,等.宁南黄土丘陵区坡向、坡位对苜蓿地土壤含水量时空变异的影响[J].水土保持研究,2010,17(2):141-144.
[26] 潘占兵,李生宝,蔡进军,等.宁南山区苜蓿地土壤水分和养分变异规律研究[J].水土保持通报,2011,31(2):61-67.
[27] 何福红,黄明斌,党廷辉.黄土高原沟壑区小流域土壤干层的分布特征[J].自然资源学报,2003,18(1):30-35.
[28] 牛俊杰,赵景波,王尚义.论山西褐土区农田土壤干燥化问题[J].地理研究,2008,27(3):519-526.
[29] 王力,邵明安,侯庆春,等.延安试区人工刺槐林地的土壤干层分析[J].西北植物学报,2001,21(1):101-106.
[30] 李玉山.旱作高产田产量波动性和土壤干燥化[J].土壤学报,2001,38(3):353-356.
[31] 郭忠升,邵明安.半干旱区人工林草地土壤旱化与土壤水分植被承载力[J].生态学报,2003,23(8):1640-1647.
[32] 王国梁,刘国彬,常欣.黄土丘陵区小流域植被建设的土壤水文效应[J].自然资源学报,2002,17(3):339-344.
[33] 万素梅,贾志宽,王勇,等.黄土高原半湿润区苜蓿草地土壤干层形成及氮素消耗研究[J].自然资源学报,2008,23(3):383-390.
[34] 杨建军,李会科,张广军,等.黄土高原土壤干层减缓方法初探[J].水土保持学报,2006,20(4):186-190.
[35] 段建军,王小利,张彩霞,等.黄土高原土壤干层评定指标的改进及分级标准[J].水土保持学报,2007,21(6):151-154.
[36] 赵景波,李瑜琴.陕西黄土高原土壤干层对植树造林的影响[J].中国沙漠,2005,25(3):370-373.
[37] 程积民,程杰,高阳.半干旱区退耕地紫花苜蓿生长特性与土壤水分生态效应[J].草地学报,2011,19(4):565-569,576.
[38] 方新宇,李军,王学春,等.黄土高原半湿润区苜蓿草地土壤干燥化与草粮轮作水分恢复效应[J].中国农业科学,2010,43(16):3348-3356.
[39] 王志强,刘宝元,路炳军.黄土高原半干旱区土壤干层水分恢复研究[J].生态学报,2003,23(9):1944-1950.
[40] 孙建,李军,王美艳,等.黄土高原半干旱偏旱区苜蓿粮食轮作土壤水分恢复效应[J].农业工程学报,2009,25(6):33-39.

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