[1] BAYAT H, RASTGO M, ZADEH M, et al. Particle size distribution models, their characteristics and fitting capability[J].Journal of Hydrology, 2015, 3(529): 872-889.[2] SHI Z H, FANG N F, WU F Z, et al. Soil erosion processes and sediment sorting associated with transport mechanisms on steep slopes[J]. Journal of Hydrology, 2012(454): 123-130.[3] HILLEL D. Fundamentals of soil physics[M]. New York: Academic Press, Inc.(New York)Ltd, 1980.[4] FILGUEIRA R R, PACHEPSKY Y A, FOURNIER L L. Timemass scaling in soil texture analysis[J]. Soil Science Society of America Journal, 2003, 67(6): 1703-1706.[5] BURGOS P, MADEJóN E, CABRERA F. Nitrogen mineralization and nitrate leaching of a sandy soil amended with different organic wastes[J].Waste Management & Research, 2006, 24(2): 175-182.[6] 禹雪中, 杨志峰, 钟德钰, 等. 河流泥沙与污染物相互作用数学模型[J]. 水利学报, 2006, 37(1): 10-15.[YU Xuezhong, YANG Zhifeng, ZHONG Deyu et al. Numerical model for interaction between sediment and pollutant in river[J]. Journal of Hydraulic Engineering, 2006, 37(1): 10-15.][7] 高建华, 欧维新, 杨桂山, 等. 苏北潮滩不同生态带沉积物分布特征[J]. 东海海洋, 2005, 23(1): 40-47.[GAO Jianhua, OU Weixin, YANG Jiashan et al. Characteristics of tidal flat sediment at different ecologic zones north Jiangsu Province[J].aDonghai Marine Science, 2005, 23(1): 40-47.][8] VISHER G S. Grain size distributions and depositional processes[J]. Journal of Sedimentary Petrology.1969, (39): 1074-1106.[9] FRIEDMAN G M. Address of the retiring president of the international association of sedimentology: difference in size distributions of populations of particles among sands from various origins[J]. Sedimentology, 1979, (26): 3-32.[10] SONG J X, CHEN X H, CHENG C, et al. Feasilibity of grainsize analysis methods for determination of vertical hydraulic conductivity of streambeds[J]. Journal of Hydrology, 2009, (375): 428-437.[11] 张锦春, 刘长仲, 姚拓, 等. 库姆它格柽柳沙包年层粒度特征及其沉积环境探讨[J]. 干旱区地理, 2014, 37(6): 1155-1162.[ZHANG Jinchun, LIU Changzhong, YAO Tuo, et al. Exploration to sedimentary environment and grain-size characteristics in age layers of Tamarix sand-hillocks in Kumtag Desert[J]. Arid Land Geography, 2014, 37(6): 1155-1162.][12] 李晓刚, 黄春长, 庞奖励. 丹江上游全新世早期古洪水滞流沉积物粒度特征研究[J]. 干旱区地理, 2014, 37(4): 646-655.[LI Xiaogang, HUANG Chunchang, PANG Jiangli. Grain-size characteristics of the early Holocene flood Slackwater deposits in the upper reaches of Danjiang River[J]. Arid Land Geography, 2014, 37(4): 646-655.][13] 刘韬, 张士锋, 刘苏峡. 十大孔兑暴雨洪水产输沙关系初探-以西柳沟为例[J]. 水资源与水工程学报, 2007, (3): 18-21.[LIU Tao, ZHANG Shifeng, LIU Suxia. Primary analysis of the relationship between storm runoff and sediment yield in Ten-watershed: a case study on Xiliu brook[J]. Journal of Water Resources&Water Engineering, 2007, (3): 18-21.][14] 许炯心.“十大孔兑”侵蚀产沙与风水两相作用及高含沙水流的关系[J]. 泥沙研究, 2013, (6): 28-37.[XU Jiongxin. Erosion and sediment yield of 10 small tributaries joining Inner Mengolia reach of upper Yellow River in relation with coupled wind-water process and hyperconcerntrated flows[J]. Journal of Sediment Research, 2013, (6): 28-37.][15] 许林军, 杨亚娟, 朱莉莉, 等. 毛不拉孔兑水土流失特征与防治布局[J]. 水土保持应用技术, 2011, (6): 32-34.[XU Linjun, YANG Yajuan, ZHU Lili et al. The characteristics of water and soil loss and conservation technology in Maobula River[J].Technology of Soil andWater Conservation, 2011, (6): 32-34.][16] FRIEDMAN G M, SANDERS J E. Principles of sedimentology[J]. New York: JohnWiley&Sons, 1978.[17] 徐树建, 潘保田, 张慧等.末次冰期旋回风成沉积物图解法与矩值法粒度参数的对比[J]. 干旱区地理, 2005, 428(2): 194-198.[XU Jianshu, PAN Baotian, ZHANG Hui et al. Grain size parameters of loess-palaeosol deposits from graphic and moment methods: a comparative study[J]. Arid Land Geography, 2005, 428(2): 194-198.][18] 黄思静. 用EXCEL计算沉积物粒度分布参数[J]. 成都理工学院学报, 1999, 26(2): 196-198.[HUANG Sijing. Calculations of grain size distribution of parameters of sediments by Microsoft excel[J]. Journal of Chengdu University of Technology, 1999, 26(2): 196-198.][19] 卢连战, 史正涛. 沉积物粒度参数内涵及计算方法的解析[J].环境科学与管理, 2010, 35(6): 54-60.[LU Lianzhan, SHI Zhengtao. Study on the grain size parameters of sediment and calculation ways[J]. Environmental Science and Management, 2010, 35(6): 54-60.][20] 牛红义, 吴群河, 陈新庚. 珠江(广州河段)表层沉积物粒度分布特征[J]. 生态环境, 2007, 16(5): 1353-1357.[NIU Hongyi, WU Qunhe, CHEN Xingeng. Grain size distribution characteristics of the surface sediments in the Pearl River(Guangzhou section)[J]. Ecology and Environment, 2007, 16(5): 1353-1357.][21] 陈冬梅, 穆桂金. 不同沉积环境下沉积物的粒度分形特征的对比研究[J]. 干旱区地理, 2004, 27(1): 47-51.[CHEN Dongmei, MU Guijin. Comparing study of grain size fractal dimensions characteristics between several sediments with different forming environments[J]. Arid Land Geography, 2004, 27(1): 47-51.][22] 武安斌. 冰碛物的粒度参数特征及其与沉积环境的关系[J].冰川冻土, 1983, 5(2): 47-53.[WU Anbin. The grain size parameters characteristics of glacial till and the relationships of sediment environment[J]. Journal of glaciology and Cryopedology, 1983, 5(2): 47-53.][23] 王翠, 雷加强, 李生宇, 等. 策勒绿洲-沙漠过渡带风沙流挟沙粒度的垂直分异[J]. 干旱区地理, 2014, 37(2): 230-238.[WANG Cu, LEI Jiaqiang, LI Shengyu et al. Vertical distribution of grain size in aeolian flow in Cele oasis-desert ecotone[J].Arid Land Geography, 2014, 37(2): 230-238.][24] 钱宁, 万兆惠. 泥沙运动力学[M]. 北京: 科学出版社, 2003.[QIAN Ning, WAN Zhaohui. Dynamics of sediment movement[M]. Beijing: Science Press, 2003.] |