1. 桂林理工大学 广西环境污染控制理论与技术重点实验室科教结合科技创新基地,广西,桂林,541004
2. 桂林理工大学 岩溶地区水污染控制与用水安全保障协同创新中心,广西,桂林,541004
纸质出版:2020
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王星, 徐勤学, 赖本忠, 等. 砾石对石灰土表面干缩裂隙发育特征的影响[J]. 水土保持通报, 2020,40(3):20-26.
Wang Xing, Xu Qinxue, Lai Benzhong, et al. Effects of Rock Fragments on Characteristics of Surface Shrinkage Cracks in Calcareous Soil[J]. Bulletin of Soiland Water Conservation, 2020, 40(3): 20-26.
王星, 徐勤学, 赖本忠, 等. 砾石对石灰土表面干缩裂隙发育特征的影响[J]. 水土保持通报, 2020,40(3):20-26. DOI: 10.13961/j.cnki.stbctb.2020.03.004.
Wang Xing, Xu Qinxue, Lai Benzhong, et al. Effects of Rock Fragments on Characteristics of Surface Shrinkage Cracks in Calcareous Soil[J]. Bulletin of Soiland Water Conservation, 2020, 40(3): 20-26. DOI: 10.13961/j.cnki.stbctb.2020.03.004.
[目的] 研究砾石粒径及含量对石灰土表面干缩裂隙发育特征的影响,为探索喀斯特地区的水土流失机理提供参考依据。[方法] 通过室内模拟试验和数字图像处理技术,研究了砾石粒径(2.0~5.0 mm和5.0~12.5 mm)和砾石含量(0%,10%,20%,30%,40%)条件下的石灰土表面干缩裂隙特征。[结果] ①无砾石石灰土平均表面裂隙率仅为3.03%,含砾石石灰土具有更大的表面裂隙率,在大粒径(5.0~12.5 mm)高含量(40%)条件下,表面裂隙率最大,达到8.66%;②当砾石含量增加时,裂隙的形态变得细小且密集,小粒径砾石会使裂隙网络更复杂;③大粒径(5.0~12.5 mm)条件下的土壤表面裂隙率与砾石含量成正线性相关,而小粒径(2.0~5.0 mm)条件下的裂隙率与砾石含量成负线性相关;④砾石会成为裂隙发育的基点,每个砾石颗粒周围都有可能产生围绕砾石或是向外延伸的裂隙。且在砾石形态的棱角处,容易产生向外延伸的裂隙。[结论] 石灰土中存在砾石会导致表面裂隙率提高,弱化土体的抗侵蚀能力,是石漠化治理不容忽视的问题。
[Objective] The effects of rock fragment (RF) size and content on the development characteristics of surface shrinkage cracks in calcareous soil were studied to provide a reference basis for exploring the mechanism of soil erosion in karst areas.[Methods] RF size (2~5 and 5~12.5 mm) and RF content (0%
10%
20%
30%
and 40%) were controlled
and digital-image-processing technology was used to study the effect of RFs on surface crack development in calcareous soil.[Results] ① The surface crack rate (SCR) of the calcareous soil without RFs was only 3.03%
whereas the samples with added RFs had a larger SCR. The maximum SCR of sample (5~12.5 mm
40%) reached 8.66%. ② When RF content increased
the morphology of the crack network became small and dense
and small RFs made the crack network more complex. ③ The SCR of 5~12.5 mm RFs was positively correlated with the RF content
whereas the SCR of 2~5 mm RFs was negatively correlated with the RF content. ④ RFs can become the basis of fracture development
and each RF probably produce fracture around the RF or extend the crack network. Moreover
at the corner of an RF
it was easy to produce cracks extending outward.[Conclusion] The existence of RFs in calcareous soil could lead to the increase of the SCR and weaken the resistance of soil to erosion.
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.
卢全中,彭建兵,陈志新,等.黄土高原地区黄土裂隙发育特征及其规律研究[J].水土保持学报,2005,19(5):191-194.
袁俊平,殷宗泽.膨胀土裂隙的量化指标与强度性质研究[J].水利学报,2004,35(6):108-113.
刘春,王宝军,施斌,等.基于数字图像识别的岩土体裂隙形态参数分析方法[J].岩土工程学报,2008,30(9):1383-1388.
冷挺,唐朝生,施斌.干湿循环条件下重塑膨胀土的裂隙发育特征及量化研究[J].工程地质学报,2016,24(5):856-862.
朱磊,马荣,范东峻,等.考虑相关长度的土壤开裂模型改进及其参数对裂隙形态的影响[J].农业工程学报,2018,34(24):123-131.
张萌,申同庆,马荣,等.作物根系影响下的农田干缩裂隙网络多重分形分析[J].灌溉排水学报,2019,38(8):45-52.
Cheng Qing, Tang Chaosheng, Zeng Hao, et al. Effects of microstructure on desiccation cracking of a compacted soil [J]. Engineering Geology, 2020,265:105418.
张家俊,龚壁卫,胡波,等.干湿循环作用下膨胀土裂隙演化规律试验研究[J].岩土力学,2011,32(9):2729-2734.
曹建华,袁道先,潘根兴.岩溶生态系统中的土壤[J].地球科学进展,2003,18(1):37-44.
Martínez-Zavala L, Jorda’n A. Effect of rock fragment cover on interrill soil erosion from bare soils in Western Andalusia, Spain [J]. Soil Use and Management, 2008,24(1):108-117.
Urbanek E, Shakesby R A. Impact of stone content on water movement in water-repellent sand [J]. European Journal of Soil Science, 2009,60(3):412-419.
Zhang Yinghu, Zhang Mingxiang, Niu Jianzhi, et al. Rock fragments and soil hydrological processes: Significance and progress [J]. Catena, 2016,147:153-166.
Cousin I, Nicoullaud B, Coutadeur C. Influence of rock fragments on the water retention and water percolation in a calcareous soil [J]. Catena, 2003,53(2):97-114.
刘建伟.桂西北喀斯特峰丛洼地石质土壤入渗试验研究[D].重庆:西南大学,2008.
Gargiulo L, Mele G, Terribile F. The role of rock fragments in crack and soil structure development: A laboratory experiment with a Vertisol [J]. European Journal of Soil Science, 2015,66(4):757-766.
曹玲,王志俭,张振华.降雨-蒸发条件下膨胀土裂隙演化特征试验研究[J].岩石力学与工程学报,2016,35(2):413-421.
周明涛,杨森,秦健坤,等.土壤裂隙研究的回顾与展望[J].土壤通报,2017,48(4):988-995.
Poesen J, Lavee H. Rock fragments in top soils: Significance and processes [J]. Catena, 1994,23(1/2):1-28.
唐朝生,王德银,施斌,等.土体干缩裂隙网络定量分析[J].岩土工程学报,2013,35(12):2298-2305.
陈尚星.基于分形理论的土体裂隙网络研究[D].南京:河海大学,2006.
DeCarlo K F, Shokri N. Effects of substrate on cracking patterns and dynamics in desiccating clay layers [J]. Water Resources Research, 2014, 50(4):3039-3051.
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