[1] AHIRWAL J, MAITI S K. Assessment of soil properties of different land uses generated due to surface coal mining activities in tropical Sal ( Shorea robusta ) forest, India [J]. Catena, 2016, 140: 155-163. [2] 宋晓波. 中国适宜露天开采的煤炭资源分布及其评价研究 [J]. 煤炭工程, 2015, 47(12): 124-126. [SONG X B. Distribution and evaluation of coal resources suitable for open-pit mining in China. Coal Engineering, 2015, 47(12): 124-126. ] [3] 魏忠义, 白中科. 露天矿大型排土场水蚀控制的径流分散概念及其分散措施 [J]. 煤炭学报, 2003, 28(5): 486-490. [WEI Z Y, BAI Z K. The concept and measures of runoff-dispersing on water erosion control in the large dump of opencast mine. Journal of China Coal Society, 2003, 28(5): 486-490. ] [4] 文月荣, 党廷辉, 唐骏, 等. 不同林地恢复模式下露天煤矿排土场土壤有机碳分布特征 [J]. 应用生态学报, 2016, 27 (1): 83-90. [WEN Y R, DANG T H, TANG J, et al. Distribution characteristics of soil organic carbon under different forest restoration modes on opencast coal mine dump. Chinese Journal of Applied Ecology, 2016, 27(1): 83-90. ] [5] 白中科, 王文英, 李晋川, 等. 黄土区大型露天煤矿剧烈扰动土地生态重建研究 [J]. 应用生态学报, 1998, 9(6): 621-626. [BAI Z K, WANG W Y, LI J C, et al. Ecological rehabilitation of drastically disturbed land at large opencut coal mine in loess area. Chinese Journal of Applied Ecology, 1998, 9(6): 621-626. ] [6] MUKHOPADHYAY S, MAITI S K, MASTO R E. Use of Reclaimed Mine Soil Index (RMSI) for screening of tree species for reclamation of coal mine degraded land [J]. Ecological Engineering, 2013, 57: 133-142. [7] RITTER J B, GARDNER T W. Hydrologic evolution of drainage basins disturbed by surface mining, central Pennsylvania [J]. Geological Society of America Bulletin, 1993, 105(1): 101-115. [8] HERAS M D L, MERINO-MARTÍN L, NICOLAU J M. Effect of vegetation cover on the hydrology of reclaimed mining soils under Mediterranean-Continental climate [J]. Catena, 2009, 77(1): 39-47. [9] BUNDT M, ALBRECHT A, FROIDEVAUX P, et al. Impact of preferential flow on radionuclide distribution in soil [J]. Environmental Science & Technology, 2000, 34(18): 209-216. [10] HENDRICKX J M H, FLURY M. Uniform and preferential flow mechanisms in the vadose zone [M]// Conceptual Models of Flow and Transport in the Fractured Vadose Zone. The National Academies Press, 2001: 149-187. [11] HAGEDORN F, BUNDT M. The age of preferential flow paths [J]. Geoderma, 2002, 108(1): 119-132. [12] FLUHLER H, DURNER W, FLURY M. Lateral solute mixing processes—A key for understanding field-scale transport of water and solutes [J]. Geoderma, 1996, 70: 165-183. [13] ZHANG Y, ZHANG M, NIU J, et al. The preferential flow of soil: A widespread phenomenon in pedological perspectives [J]. Eurasian Soil Science, 2016, 49(6): 661-672. [14] GERMANN P, BEVEN K. Water flow in soil macropores I: An experimental approach [J]. European Journal of Soil Science, 1981, 32: 1-13. [15] NOGUCHI S, NIK A R, KASRAN B, et al. Soil physical properties and preferential flowpaths in tropical rainforest, Bukit Tarek, Peninsular Malaysia [J]. Journal of Forest Research, 1997, 2(2): 115-120. [16] STEWART J B, MORAN C J, WOOD J T. Macrospore sheath: Quantification of plant root and soil macrospore association [J]. Plant & Soil, 1999, 211(1): 59-67. [17] JØRGENSEN P R, HOFFMANN M, KISTRUP J P, et al. Preferential flow and pesticide transport in a clay-rich till: Field, laboratory, and modeling analysis [J]. Water Resources Research, 2002, 38(11): 28-1-28-15. doi:10.1029/2001WR000494. [18] DUSEK J, VOGEL T, LICHNER L, et al. Simulated cadmium transport in macrospores soil during heavy rainstorm using dual-permeability approach [J]. Biologia, 2006, 61(19): S251-S254. [19] YAN J, ZHAO W. Characteristics of preferential flow during simulated rainfall events in an arid region of China [J]. Environmental Earth Sciences, 2016, 75(7): 1-12. [20] 闫加亮, 赵文智, 张勇勇. 绿洲农田土壤优先流特征及其对灌溉量的响应 [J]. 应用生态学报, 2015, 26(5): 1454-1460. [YAN J L, ZHAO W Z, ZHANG Y Y. Characteristics of the preferential flow and its response to irrigation amount in oasis cropland. Chinese Journal of Applied Ecology, 2015, 26(5): 1454-1460. ] [21] MATTHEWS A M, ARMSTRONG A C, LEEDS-HARRISON P B, et al. Development and testing of a model for predicting tillage effects on nitrate leaching from cracked clay soils [J]. Soil & Tillage Research, 2000, 53(3): 245-254. [22] SHIPITALO M J, NUUTINEN V, BUTT K R. Interaction of earthworm burrows and cracks in a clayey, subsurface-drained, soil [J]. Applied Soil Ecology, 2004, 26(3): 209-217. [23] 张中彬, 彭新华. 土壤裂隙及其优先流研究进展 [J]. 土壤学报, 2015, 52(3): 477-488. [ZHANG Z B, PEGN X H. A review of researches on soil cracks and their impacts on preferential flow. Acta Pedologica Sinica, 2015, 52(3): 477-488. ] [24] GUEBERT M D, GARDNER T W. Macropore flow on a reclaimed surface mine: Infiltration and hillslope hydrology [J]. Geomorphology, 2001, 39(3/4): 151-169. [25] HANGEN E, GERKE H H, SCHAAF W, et al. Flow path visualization in a lignitic mine soil using iodine-starch staining [J]. Geoderma, 2004, 120(1/2): 121-135. [26] GARRIDO F, SERRANO S, BARRIOS L, et al. Preferential flow and metal distribution in a contaminated alluvial soil from São Domingos mine (Portugal) [J]. Geoderma, 2014, 213: 103-114. [27] CLARK E V, ZIPPER C E. Vegetation influences near-surface hydrological characteristics on a surface coal mine in eastern USA [J]. Catena, 2016, 139: 241-249. [28] HANGEN E, GERKE H H, SCHAAF W, et al. Assessment of preferential flow processes in a forest-reclaimed lignitic mine soil by multicell sampling of drainage water and three tracers [J]. Journal of Hydrology, 2005, 303(1): 16-37. [29] 李文银,王治国,蔡继清. 工矿区水土保持 [M]. 北京: 科学出版社, 1996: 29-30. [LI W Y, WANG Z G, CAI J Q. Water and Soil Conservation in Industrial and Mining Areas. Beijing: Science Press, 1996: 29-30. ] [30] ZHANG H, CHENG J, SHI Y, et al. The distribution of preferential paths and its relation to the soil characteristics in the Three Gorges Area, China [J]. International Journal of Sediment Research, 2007, 22(1): 39-48. [31] 王丽艳, 韩有志, 张成梁, 等. 不同植被恢复模式下煤矸石山复垦土壤性质及煤矸石风化物的变化特征 [J]. 生态学报, 2011, 31(21): 6429-6441. [WANG L Y, HAN Y Z, ZHANG C L, et al. Reclaimed soil properties and weathered gangue change characteristics under various vegetation types on gangue pile. Acta Ecologica Sinica, 2011, 31(21): 6429-6441. ] [32] ZAVALA L M, GONZÁLEZ F A, JORDÁN A. Fire-induced soil water repellency under different vegetation types along the Atlantic dune coast-line in SW Spain [J]. Catena, 2009, 79(2): 153-162. [33] KOESTEL J K, MOEYS J, JARVIS N J. Meta-analysis of the effects of soil properties, site factors and experimental conditions on solute transport [J]. Hydrology & Earth System Sciences Discussions, 2012, 16(6): 1647-1665. [34] 吕文星. 三峡库区三种土地利用方式优先流特征及其对硝态氮运移的影响 [D]. 北京: 北京林业大学, 2013. [LÜ W X. Characteristics of Preferential Flow and Its Effect on Nitrate Nitrogen Transport in Three Land Use Types of the Three Gorges Reservoir Area. Beijing: Beijing Forestry University, 2013. ] [35] WANG Q, YANG W, LIU W. Adsorption of acetanilide herbicides on soils and its correlation with soil properties [J]. Pesticide Science, 1999, 55(11): 1103-1108. [36] HERRICK J E, ZEE J W V, BELNAP J, et al. Fine gravel controls hydrologic and erodibility responses to trampling disturbance for coarse-textured soils with weak cyanobacterial crusts [J]. Catena, 2010, 83(2/3): 119-126. [37] ZAVALA L M, JORDÁN A, BELLINFANTE N, et al. Relationships between rock fragment cover and soil hydrological response in a Mediterranean environment [J]. Soil Science & Plant Nutrition, 2010, 56(1): 95-104. [38] JOMAA S, BARRY D A, BROVELLI A, et al. Rain splash soil erosion estimation in the presence of rock fragments [J]. Catena, 2012, 92: 38-48. [39] EDWARDS W M, SHIPITALO M J, OWENS L B, et al. Rainfall intensity affects transport of water and chemicals through macrospores in no-till soil [J]. Soil Science Society of America Journal, 1992, 56(1): 52-58. [40] 张英虎, 牛健植, 朱蔚利, 等. 森林生态系统林木根系对优先流的影响 [J]. 生态学报, 2015, 35(6): 1788-1797. [ZHANG Y H, NIU J Z, ZHU W L, et al. Effects of plant root systems on preferential flow in forest ecosystems. Acta Ecologica Sinica, 2015, 35(6): 1788-1797. ] |