[1] 袁晓宇,海春兴,刘广通.阴山北麓不同用地土壤有机质含量对抗风蚀的作用研究[J].水土保持研究,2007,14(6):306-308. [Yuan Xiaoyu,Hai Chunxing,Liu Guangtong.Influence of different soil organic matters on resistance to wind erosion in North foot of the Yinshan Mountain[J].Research of Soil and Water Conservation,2007,14(6):306-308.] [2] 苏永中,赵哈林,文海燕.退化沙质草地开垦和封育对土壤理化性状的影响[J].水土保持学报,2002,16(4):5-8. [Su Yongzhong,Zhao Halin,Wen Haiyan.Cultivation and enclosure effects on soil physicochemical properties of degraded sandy grassland[J].Journal of Soil and Water Conservation,2002,16(4):5-8.] [3] 吴建国,张小全,王彦辉,等.土地利用变化对土壤物理组分中有机碳分配的影响[J].林业科学,2002,38(4):19-29. [Wu Jianguo,Zhang Xiaoquan,Wang Yanhui,et al.The effects of land use changes on the distribution of soil organic carbon in physical fractionation of soil[J].Scientia Silvae Sinicae,2002,38(4):19-29.] [4] 赵哈林,周瑞莲,苏永中,等.科尔沁沙地沙漠化过程中土壤有机碳和全氮含量变化[J].生态学报,2008,28(3):976-982. [Zhao Halin,Zhou Ruilian,Su Yongzhong,et al.Changes of soil organic cand total in contents as affected by desertification in Horqin Sandland,North China[J].Acta Ecologica Sinica,2008,28(3):976-982.] [5] 杨钦,郭中领,王仁德,等.河北坝上不同土地利用方式对土壤风蚀的影响[J].干旱区资源与环境,2017,31(2):185-190. [Yang Qin,Guo Zhongling,Wang Rende,et al.Influence of different land uses on soil wind erosion in Bashang area,Hebei,China[J].Journal of Arid Land Resources and Environment,2017,31(2):185-190.] [6] 赵哈林,周瑞莲,赵学勇,等.呼伦贝尔沙质草地土壤理化特性的沙漠化演变规律及机制[J].草业学报,2012,21(2):1-7. [Zhao Halin,Zhou Ruilian,Zhao Xueyong,et al.Desertification mechanisms and process of soil chemical land physical properties in Hulunbeir sandy grassland,Inner Mongolia[J].Acta Pratacultura Sinica,2012,21(2):1-7.] [7] 李海东,沈渭寿,邹长新,等.雅鲁藏布江山南宽谷风沙化土地土壤养分和粒度特征[J].生态学报,2012,32(16):4981-4992. [Li Haidong,Shen Weishou,Zou Changxin,et al.Soil nutrients content and grain size fraction of aeolian sandy land in the Shannan wide valley of the Yarlung Zangbo River,China[J].Acta Ecologica Sinica,2012,32(16):4981-4992.] [8] 高君亮,高永,罗凤敏,等.表土粒度特征对风蚀荒漠化的响应[J].科技导报,2014,32(25):20-25. [Gao Junliang,Gao Yong,Luo Fengmin,et al.Response of surface soil grain size characteristics to wind erosion desertification[J].Science & Technology Review,2014,32(25):20-25.] [9] 杨永胜.毛乌素沙地生物结皮对土壤水分和风蚀的影响[D].杨凌:西北农林科技大学,2012. [Yang Yongsheng.Effects of Biological Soil Crusts on Soil Mmoisture and Wind Erosion in Mu Us Sandland[D].Yangling:Northwest A & F University,2012.] [10] 符超峰,赵景波.毛乌素沙地东南缘不同类型沙丘土壤水分分布特征[J].干旱区研究,2011,28(3):377-383. [Fu Chaofeng,Zhao Jingbo.Distribution of soil moisture content in different types of sand dunes in the Southeastern marginal zone of the Mu Us Sandy Land[J].Arid Zone Research,2011,28(3):377-383.] [11] 王志,王蕾,刘连友,等.毛乌素沙地南缘沙丘水分的时空分布特征[J].干旱区研究,2007,24(1):61-65. [Wang Zhi,Wang Lei,Liu Lianyou,et al.Preliminary study on spatiotemporal distribution of moisture contents in sand dunes in the Southern marginal zone of the Mu Us Desert[J].Arid Zone Research,2007,24(1):61-65.] [12] 杨梅焕,曹明明,朱志梅,等.毛乌素沙地沙漠化过程中土壤理化性质分析[J].水土保持通报,2010,30(2):169-172. [Yang Meihuan,Cao Mingming,Zhu Zhimei,et al.Soil physical and chemical properties in the process of desertification on the Southeastern edge of Mu Us Sand Land[J].Bulletin of Soil and Water Conservation,2010,30(2):169-172.] [13] 雷金银,吴发启,马璠,等.毛乌素沙地土壤风蚀的气候因子分析[J].水土保持研究,2007,14(2):104-105. [Lei Jinyin,Wu Faqi,Ma Fan,et al.The analysis of climate factors effecting wind erosion in Maowusu Sandy Land[J].Research of Soil and Water Conservation,2007,14(2):104-105.] [14] 黄富祥,牛海山,王明星,等.毛乌素沙地植被覆盖率与风蚀输沙率定量关系[J].地理学报,2001,56(6):700-710. [Huang Fuxiang,Niu Haishan,Wang Mingxing,et al.The relationship between vegetation cover and sand transport flux at Mu Us Sandland[J].Acta Geographica Sinica,2001,56(6):700-710.] [15] 朱震达,吴正,刘恕,等.中国沙漠概论[M].修订版.北京:科学出版社,1981. [Zhu Zhenda,Wu Zheng,Liu Shu,et al.Introduction to Chinese Desert[M].Revised Edition.Beijing:Science Press,1981.] [16] 杨永梅,杨改河,冯永忠.近45年毛乌素沙地的气候变化及其与沙漠化的关系[J].西北农林科技大学学报(自然科学版),2007,35(12):87-92. [Yang Yongmei,Yang Gaihe,Feng Yongzhong.Climatic variation and its effect on desertification in 45 recent years in Mu Us sandland[J].Journal of Northwest A & F University(Natural Science Edition),2007,35(12):87-92.] [17] 徐丹丹,尹立河,侯光才,等.毛乌素沙地旱柳和小叶杨树干液流密度及其与气象因子的关系[J].干旱区研究,2017,34(2):375-382. [Xu Dandan,Yin Lihe,Hou Guangcai,et al.Relationships between sap flow densities in tree trunks of Salix matsudana and Populus simonii and meteorological factors in the Mu Us Sand-land[J].Arid Zone Research,2017,34(2):375-382.] [18] 张惜伟,汪季,高永,等.呼伦贝尔沙质草原风蚀坑表层土壤粒度特征[J].干旱区研究,2017,34(2):293-299. [Zhang Xiwei,Wang Ji,Gao Yong,et al.Grain size characteristics of topsoil in blowouts on sandy grasslands in Hulun Buir[J].Arid Zone Research,2017,34(2):293-299.] [19] 成都地质学院陕北队.沉积岩(物)粒度分析及其应用[M].北京:地质出版社,1978:46-56. [Chengdu Academy of Geology,North Shaanxi Team.Particle Size Analysis of Sedimentary Rocks and Its Application[M].Beijing:Geological Publishing House,1978:46-56.] [20] 南京农学院.土壤农化分析[M].北京:农业出版社,1985:31-52. [Nanjing College of Agriculture.Soil and Agriculture Chemistry Analysis[M].Beijing:Agriculture Press,1985:31-52.] [21] 苏永中,赵哈林.农田沙漠化过程中土壤有机碳和氮的衰减及其机理研究[J].中国农业科学,2003,36(8):928-934. [Su Yongzhong,Zhao Halin.Losses of soil organic carbon and nitrogen and their mechanisms in the desertification process of sandy farmlands in Horqin Sandy Land[J].Scientia Agricultura Sinica,2003,36(8):928-934.] [22] 李占宏,海春兴,丛艳静.毛乌素沙地表土粒度特征及其空间变异[J].中国水土保持科学,2009,7(2):74-79. [Li Zhanhong,Hai Chunxing,Cong Yanjing.Topsoil particle-size distribution and its spatial variation in Mu Us Desert[J].Science of Soil and Water Conservation,2009,7(2):74-79.] [23] 舒培仙,牛东风,李保生,等.毛乌素沙地现代沙丘沙的粒度特征及其意义[J].中国沙漠,2016,36(1):158-166. [Shu Peixian,Niu Dongfeng,Li Baosheng,et al.Grain size characteristics of modern dune sand and its significance in the Mu Su Sandy Land,China[J].Journal of Desert Research,2016,36(1):158-166.] [24] 沈亚萍,张春来,李庆,等.中国东部沙区表层沉积物粒度特征[J].中国沙漠,2016,36(1):150-157. [Shen Yaping,Zhang Chunlai,Li Qin,et al.Grain-size characteristics of surface sediments in the Eastern Desert Regions of China[J].Journal of Desert Research,2016,36(1):150-157.] [25] 杨志勇,陈新闯,郭建英,等.乌兰布和沙漠不同土地利用类型粒度特征分析[J].中国水土保持,2015(7):50-53. [Yang Zhiyong,Chen Xinchuang,Guo Jianying,et al.Grain size characteristics of different land use types in Ulanbuh Desert[J].Soil and Water Conservation in China,2015(7):50-53.] [26] 张志栋,常春平,郭中领,等.河北坝上农田、退耕地和天然草地土壤的可风蚀性[J].中国沙漠,2018,38(1):85-91. [Zhang Zhidong,Chang Chunping,Guo Zhongling,et al.Soil Wind erodibility of farmland,abandonded farmland and glassland in the Bashang Area of Hebei,China[J].Journal of Desert Research,2018,38(1):85-91.] [27] 刘目兴,刘连友.农田休闲期作物留茬对近地表风场的影响[J].农业工程学报,2009,25(9):295-300. [Liu Muxing,Liu Lianyou.Effect of crop stubble on wind field above field surface during fallow period of cropland[J].Transactions of the CSAE,2009,25(9):295-300.] [28] 董光荣,李长治,金炯,等.关于土壤风蚀风洞模拟实验的某些结果[J].科学通报,1987,32(4):297-301. [Dong Guangrong,Li Changzhi,Jin Jiong,et al.Some results on wind tunnel simulation experiments of soil erosion[J].Science Bulletin,1987,32(4):297-301.] [29] 庞营军,屈建军,牛清河,等.敦煌月牙泉景区沙丘表面沙物质的粒度特征[J].干旱区研究,2017,34(3):701-706. [Pang Yingjun,Qu Jianjun,Niu Qinghe,et al.Grain size characters of dune surface sediment in the crescent spring scenic spot,Dunhuang[J].Arid Zone Research,2017,34(3):701-706.] [30] 王清奎,汪思龙,高洪,等.土地利用方式对土壤有机质的影响[J].生态学杂志,2005,24(4):6-9. [Wang Qingkui,Wang Silong,Gao Hong,et al.Influence of land use on soil organic matter[J].Chinese Journal of Ecology,2005,24(4):6-9.] [31] 乔有明,王振群,段中华.青海湖北岸土地利用方式对土壤碳氮含量的影响[J].草业学报,2009,18(6):105-112. [Qiao Youming,Wang Zhenqun,Duan Zhonghua.Effect of different land-use types on soil carbon and nitrogen contents in the Northern Region of Qinghai Lake[J].Acta Prataculturae Sinica,2009,18(6):105-112.] [32] Six J,Christian Feller,Karolien Denef,et al.Soil organic matter, biota and aggregation in temperate and tropical soils:Effects of no-tillage[J].Agronomic,2002,22:755-775. [33] Haider K,Kastanienallee,Guggenberger.Soil minerals and organic components:Impact on biological processes,human welfare and nutrition[J].Thailand,2002,8:314-321. [34] Feller C,Beare M H.Physical control of soil organic matter dynamics in the tropics[J].Geoderma,1997,79:69-116. [35] Hassink J.The capacity of soils to preserve organic C and N by their association with clay and silt particles[J].Plant Soil,1997,191:77-87. |