湖南科技大学学报(自然科学版)
湖南科技大學學報(自然科學版)
호남과기대학학보(자연과학판)
JOURNAL OF HUNAN UNIVERSITY OF SCIENCE & TECHNOLOGY(NATURAL SCIENCE EDITION)
2014年
4期
54-59
,共6页
曹运江%黄玉凤%戴世鑫%杨浩%王洪磊%潘书华%朱继良%曹修定%罗福义
曹運江%黃玉鳳%戴世鑫%楊浩%王洪磊%潘書華%硃繼良%曹脩定%囉福義
조운강%황옥봉%대세흠%양호%왕홍뢰%반서화%주계량%조수정%라복의
震前震后%泥石流%物源类型%物源量%冷木沟
震前震後%泥石流%物源類型%物源量%冷木溝
진전진후%니석류%물원류형%물원량%랭목구
before and after earthquake%debris flow%material source type%material source reserves%Lengmugou
研究区受“5.12”汶川地震、“8.18”泥石流、“4.20”芦山地震等大型地质灾害叠加作用的影响,区域上构成独特的工程地质环境条件.通过系统调研和收集宝兴冷木沟地震前后泥石流物源地质原型和泥石流灾害防治的第一手资料,重点查清泥石流形成的物源条件,对比研究“4.20”芦山地震前后泥石流物源特征、动/静储量比例.分析研究结果表明冷木沟发育点状物源、线状物源、面状物源,其中震前震后均以沟床侵蚀物源(线状物源)为主,占76.110%和60.690%.“4.20”芦山地震后,沟岸堆积物源(点状物源)却成倍增多,为48的倍率,超31.490个百分点.整体上,除沟岸侧蚀物源(面状物源)外,同一流域段内,震后物源动储量高于震前.静动储量线性关系较为明显,相关系数R2达0.8~1.0,均属高度正相关.
研究區受“5.12”汶川地震、“8.18”泥石流、“4.20”蘆山地震等大型地質災害疊加作用的影響,區域上構成獨特的工程地質環境條件.通過繫統調研和收集寶興冷木溝地震前後泥石流物源地質原型和泥石流災害防治的第一手資料,重點查清泥石流形成的物源條件,對比研究“4.20”蘆山地震前後泥石流物源特徵、動/靜儲量比例.分析研究結果錶明冷木溝髮育點狀物源、線狀物源、麵狀物源,其中震前震後均以溝床侵蝕物源(線狀物源)為主,佔76.110%和60.690%.“4.20”蘆山地震後,溝岸堆積物源(點狀物源)卻成倍增多,為48的倍率,超31.490箇百分點.整體上,除溝岸側蝕物源(麵狀物源)外,同一流域段內,震後物源動儲量高于震前.靜動儲量線性關繫較為明顯,相關繫數R2達0.8~1.0,均屬高度正相關.
연구구수“5.12”문천지진、“8.18”니석류、“4.20”호산지진등대형지질재해첩가작용적영향,구역상구성독특적공정지질배경조건.통과계통조연화수집보흥랭목구지진전후니석류물원지질원형화니석류재해방치적제일수자료,중점사청니석류형성적물원조건,대비연구“4.20”호산지진전후니석류물원특정、동/정저량비례.분석연구결과표명랭목구발육점상물원、선상물원、면상물원,기중진전진후균이구상침식물원(선상물원)위주,점76.110%화60.690%.“4.20”호산지진후,구안퇴적물원(점상물원)각성배증다,위48적배솔,초31.490개백분점.정체상,제구안측식물원(면상물원)외,동일류역단내,진후물원동저량고우진전.정동저량선성관계교위명현,상관계수R2체0.8~1.0,균속고도정상관.
“5.12”Wenchuan earthquake ,“8.18”debris flow,“4.20”Lushan earthquake and other large-scale geological disasters made additive effects on the study area,and constituted a unique engineering geological environmental condition.Through systematically investigate and collect geological prototype research of the debris flow material source before and after Lengmugou earthquake,Baoxing country and first -hand information of debris flow disaster prevention and control,the point research of the source condition of debris flow and comparative research before and after the "4.20"Lushan earthquake debris flow material source characteristics,dynamic and static material source reserve ratio,according to material source is one of the three conditions formed debris flow.The analysis results indicate that Lengmugou point material source,line material source and surface material source has well -developed,but the major is gully erosion source material (line material source),reaches 76.110% and 60.690% before and after earthquake.After Lushan earthquake, during the accumulation material source in shore ditch (point material source)increased exponentially,ratio of 48,by more than 31.490%.In addition to ditch shore erosion source material source (surface material source), dynamic reserves than before the earthquake source in the same watershed section.Static and dynamic material source reserves of linear relationship is relatively obvious,the correlation coefficient (R2 )of 0.8 ~1 .0,are positively related,and is highly relevant.