参考文献/References:
[1] 王裕宜, 田冰, 詹钱登,等. 不同权重的前期和始发日降雨量与泥石流产沙规模的分析——特大型泥石流灾害发生的思考[J]. 中国地质灾害与防治学报, 2009, 20(1): 32-38[Wang Yuyi, Tian Bing, Zhan Qiandeng, et al. Analysis of the relationship between different weight of precedent and daily critical rainfall and sediment transport scale in debris flows[J]. The Chinese Journal of Geological Hazard and Control, 2009, 20(1): 32-38]
[2] 常鸣,唐川. 基于水动力的典型矿山泥石流运动模式研究[J]. 水利学报, 2014,45(11): 1318-1326[Chang Ming, Tang Chuan. Study on typical movement model in mine debris flow based on hydrodynamic force conditions[J]. Journal of Hydraulic Engineering, 2014,45(11): 1318-1326]
[3] 江锦红,邵利萍. 基于降雨观测资料的山洪预警标准[J]. 水利学报,2010,41(4): 458-463[Jiang Jinhong, Shao Liping. Standard of mountain flood warning based on the precipitation observation data[J]. Journal of Hydraulic Engineering, 2010,41(4): 458-463]
[4] 张金山,崔鹏. 泥石流预警及其实施方法[J]. 水利学报,2012, 43(S2): 174-180[Zhang Jinshan,Cui Peng. Research on and implementation of debrisflow forecast and warning[J]. Journal of Hydraulic Engineering, 2012,43(S2): 174-180]
[5] Hu K, Cui P, Wang C, et al. Characteristic rainfall for warning of debris flows[J]. Journal of Mountain Science, 2010, 7: 207-214
[6] 陈晓清. 滑坡转化泥石流起动机理试验研究[D].成都:西南交通大学,2006:18-27[Chen Xiaoqing. Experiment of Initiation Mechanism of Landslide Translation to Debris Flow[D]. Chengdu:Southwest Jiaotong University, 2006:18-27]
[7] 胡明鉴,汪稔. 蒋家沟流域暴雨滑坡泥石流共生关系试验研究[J]. 岩石力学与工程学报,2003,22(5): 824-828[Hu Mingjian, Wang Ren. Testing study on the correlation among landslide, debris flow and rainfall in Jiangjia valley[J]. Chinese Journal of Rock Mechanics and Engineering, 2003, 22(5): 824-828]
[8] 周小军,崔鹏,李战鲁. 泥石流源区砾石土渗透沉降综合测试设备研制及应用[J]. 岩石力学与工程学报,2012,31(6): 1281-1289[Zhou Xiaojun, Cui Peng, Li Zhanlu. Development and application of integrated test equipment for permeability and settlement of gravelly soil in triggering area of debris flow[J]. Chinese Journal of Rock Mechanics and Engineering, 2012,31(6): 1281-1289]
[9] 陈中学,汪稔,胡明鉴,等. 黏土颗粒含量对蒋家沟泥石流启动影响分析[J]. 岩土力学,2010,31(7): 2197-2201[Chen Zhongxue, Wang Ren, Hu Mingjian,et al. Study of content of clay particles for debris flow occurrence in Jiangjia Ravine[J]. Rock and Soil Mechanics, 2010, 31(7): 2197-2201]
[10] 陈中学,汪稔,胡明鉴,等. 云南东川蒋家沟泥石流形成内因初探[J]. 岩土力学,2009,30(10): 3053-3056+3070[Chen Zhongxue, Wang Ren, Hu Mingjian, et al. Study of internal factors for debris flow occurrence in Jianjia Ravine, Dongchun of Yunnan[J]. Rock and Soil Mechanics, 2009, 30(10): 3053-3056+3070]
[11] 王志兵,汪稔,胡明鉴,等. 蒋家沟砾石土的特性及其对斜坡失稳的意义[J]. 岩土力学,2010,31(S2): 206-211[Wang Zhibing, Wang Ren, Hu Mingjian,et al. Characteristics of gravelly soil and their implications for slope instability in Jiangjiagou ravine[J]. Rock and Soil Mechanics, 2010, 31(S2): 206-211]
[12] Chen NS, Zhou W, Yang CL, et al. The processes and mechanism of failure and debris flow initiation for gravel soil with different clay content[J]. Geomorphology, 2010, 121(3-4): 222-230
[13] 柏春广,王建. 一种新的粒度指标:沉积物粒度分维值及其环境意义[J]. 沉积学报,2003,21(2): 234-239[Bai Chunguang, Wang jian. A new grainsize index: grainsize fractal dimension of sediment and its environmental significance[J]. Acta Sedimentologica Sinica, 2003,21(2): 234-239]
[14] 倪化勇,吕学军,杨德伟. 川藏公路培龙沟路段堆积物的分形特征及其地质意义[J]. 工程地质学报,2005,13(4): 451-454[Ni Huayong, Lv Xuejun, Yang Dewei. Fractal feature and geological significance of accumulations at Peilong section along Sichuan-Tibet highway[J]. Journal of Engineering Geology, 2005, 13(4): 451-454]
[15] May C L, Gresswell R E. Spatial and temporal patterns of debrisflow deposition in the Oregon Coast Range, USA [J]. Geomorphology, 2004, 57(3-4): 135-149
[16] 吴中如,潘卫平. 分形几何理论在岩土边坡稳定性分析中的应用[J]. 水利学报,1996,4: 79-82[Wu Zhongru, Pan Weiping. Application of fractal geometry theory in stability analysis of rock and soil slope[J]. Journal of Hydraulic Engineering, 1996,4: 79-82]
[17] 张季如,祝杰,黄丽,等. 固结条件下软黏土微观孔隙结构的演化及其分形描述[J]. 水利学报,2008,39(4):394-400[Zhang Jiru, Zhu Jie, Huang Li, et al. Evolution of micro pore structure of soft clay and its fractal features under consolidation[J]. Journal of Hydraulic Engineering, 2008,39(4):394-400]
[18] 陈颙. 分形几何学[M]. 北京: 地震出版社, 1998:22-31[Chen Yu. Fractal geometry[M]. Beijing: Seismological Press,1998:22-31]
[19] 贺拿,陈宁生,朱云华,等. 泥石流源区砾石土分形特征及其与渗透系数关系试验研究[J]. 岩土力学, 2014,35(9): 2543-2548[He Na, Chen Ningsheng, Zhu Yunhua, et al. Experiment study of fractal feature and relationship between fractal dimension and permeability coefficient of gravelly soil in debris flow source area[J]. Rock and Soil Mechanics, 2014,35(9): 2543-2548]
相似文献/References:
[1]黄祺,陈宁生,朱云华,等.泥石流源区砾石土的粒度分形特征[J].山地学报,2012,(05):578.
HUANG Qi,CHEN Ningsheng,ZHU Yunhua,et al.Particle Size Fractal Characteristics of the Gravel Soil in Original Area of Debris Flow Valleys[J].Mountain Research,2012,(01):578.
[2]陈宁生,张军.泥石流源区弱固结砾石土的渗透规律[J].山地学报,2001,(02):169.
[3]王小丹,刘刚才,刘淑珍,等.西藏高原干旱半干旱区土壤分形特征及其应用[J].山地学报,2003,(S1):58.
[4]尚正永,白永平.丘陵山区城镇体系的分形特征──以江西省赣州市为例[J].山地学报,2007,(02):142.