Results 41 to 50 of about 1,325 (153)

短历时强降雨对典型喀斯特坡耕地侵蚀产沙的影响

open access: yesShuitu Baochi Xuebao, 2019
探索短历时强降雨对典型喀斯特坡耕地侵蚀产沙的影响,为喀斯特区坡耕地应对极端天气的水土流失防治提供理论依据。研究采用人工室内模拟降雨试验的方法,对喀斯特坡耕地侵蚀产沙特征在短历时强降雨作用下的影响因素开展研究。结果表明:(1)短历时强降雨导致喀斯特坡耕地地表输沙模数和产沙量随降雨强度的增大而增大,而地下输沙模数和产沙量与降雨强度无明显变化规律,坡耕地土壤侵蚀以地表为主。地表产沙临界雨强为30~50 mm/h。(2)坡度增大时地表产沙比重大于地下产沙比重,地表土壤侵蚀以地表为主 ...
任青青   +6 more
doaj  

侵蚀性降雨标准研究

open access: yesShuitu Baochi Xuebao, 2000
建立侵蚀性降雨标准,是为了区分发生和不发生侵蚀和降雨事件,从而大大减少计算降雨侵蚀力的工作量,并提高土壤侵蚀预报精度。利用陕西团山沟小流域及所在3个小区1961-1969年的降雨过程资料,以漏选和多选降雨事件的降雨侵蚀力相等为原则,分别建立了黄土高原坡面侵蚀的侵蚀性降雨雨量标准12mm,平均雨强标准0.04mm/min,最大30min雨强标准0.25mm/min。其中时段雨强标准筛选精度最高,可剔除88%以上的降雨事件,只有5.3%的错选度。其次是平均雨强标准,雨量标准筛选精度最差 ...
谢云 刘宝元 等
doaj   +2 more sources

暴雨诱发滑坡的高效无网格大变形数值模拟 [PDF]

open access: yes, 2010
渗流与土体的大变形耦合损伤破坏问题是暴雨诱发滑坡数值模拟的重要内容,目前对滑坡的全过程大变形非线性损伤破坏的仿真分析仍是一个难点。本文基于稳定节点积分再生核质点伽辽金无网格法和大变形增量型本构关系,提出了一套能模拟暴雨诱发非饱和土质边坡大变形损伤破坏的高效分析方法。该方法应用拉格朗日稳定节点积分,保证了数值积分的稳定性和高效性;同时采用非饱和土的物理力学性质来模拟降雨过程中边坡土体性质的演化,并以各项同性损伤函数和Drucker-Prager屈服准则反映土体的弹塑性损伤状态 ...
李凌, 王东东
core  

Exploration and practice of integrated construction of meteorological risk warning for geological hazards in Zhejiang Province [PDF]

open access: yes
Geological hazard forecasting and early warning are crucial measures for preventing geological disasters and minimizing casualties. Since the initiation of geological hazard meteorological risk early warning in 2003, 80% of mountainous provinces, cities ...
Fenghua YU   +5 more
core   +1 more source

Analysis of the rainfall threshold for post-fire debris flow initiation: A case study of the debris flow at Ren’eyong gully in Xiangcheng County, Sichuan Province [PDF]

open access: yes
In the early summer of 2014, a wildfire ravaged the Ren’eyong valley in the central Mt. Hengduan region of southwestern China. Following the blaze, debris flows were triggered three times in branch No. 3 due to short-term, low intensity rainfall.
Guisheng HU   +4 more
core   +1 more source

Analysis of the characteristics and development trends of the “7•5” catastrophic debris flow in Xiangjiao gully, Muli County, Sichuan [PDF]

open access: yes
On July 5, 2021, a catastrophic debris flow disaster occured in Xiangjiao gully, Muli County, Sichuan Province. This study analyzed the formation conditions, eruption process and eruption characteristics of the debris flow through field investigation and
Hao SUN   +4 more
core   +1 more source

降雨强度和坡度对黑土区土质道路路面侵蚀特征的影响

open access: yesShuitu Baochi Xuebao, 2017
选取3种东北黑土区有代表性的侵蚀性降雨(60,90,120 mm/h)和3个典型坡度(3°,5°和7°),采用模拟降雨试验方法,研究不同降雨强度和坡度下黑土区土质道路路面径流量、侵蚀量以及产流产沙过程的变化特征。结果表明:不同降雨强度和坡度试验处理的径流量主要变化于56.3~61.8 mm;而路面侵蚀速率随降雨强度和坡度的增加分别增大1.8~11.0倍和1.2~10.0倍,且二者相互促进,共同影响土质道路路面土壤侵蚀。此外,降雨强度对黑土区土质道路路面产流率变化过程的影响明显,而坡度的影响较小 ...
沈海鸥   +5 more
doaj  

Study on rainfall landslide simulation experiment and meso evolution of soil failure of granite residual soils in Xiamen area [PDF]

open access: yes, 2014
我国东南沿海经济开放区主要分布在花岗岩风化壳上,该区域残积土厚度较大,其中在闽粤沿海地区一般为20-35m。福建省地处东南沿海,位于亚热带东南季风气候区,中低山和丘陵占全省面积的80%,气候湿热,台风暴雨频繁,降雨集中,岩土渗流强度大,丘陵山地风化与侵蚀作用强烈,导致花岗岩残积土广泛覆盖,其中50%分布在闽东南丘陵、沿海平原等地,其中厦门地区最厚达50-70m。因此,花岗岩残积土在东南部省份普遍存在,工程中所遇的山地、丘陵、剥蚀准平原上都分布着残积土,是大部分工程建设的地基基础和地质环境重要介质 ...
郑晓栩
core  

Seepage characteristics of accumulation landslides under different types of heavy rainfall stability analysis [PDF]

open access: yes
Heavy rainfall is a major causes of sedimentary landslide disasters, and understanding the spatiotemporal dynamic characteristics of the seepage field in landslides under heavy rain is crucial for evaluating landslide stability and providing ...
Hao SHI   +5 more
core   +1 more source

Response of Runoff and Sediment Yield from Maize Slope Farmland in Karst Areas to Slope Gradient [PDF]

open access: yes
[Objective] To elucidate the responses of surface runoff, subsurface runoff, and underground runoff hydrological pathways to slope in maize sloping farmland in Karst regions.
DAI Quanhou   +4 more
core   +1 more source

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