鲁东大学学报(自然科学版)
魯東大學學報(自然科學版)
로동대학학보(자연과학판)
LUDONG UNIVERSITY JOURNAL(NATURAL SCIENCE EDITION)
2015年
2期
156-161
,共6页
崔钰磊%王庆%金秉福%战超%刘鹏
崔鈺磊%王慶%金秉福%戰超%劉鵬
최옥뢰%왕경%금병복%전초%류붕
遥感%莱州湾%海岸线%地貌演变
遙感%萊州灣%海岸線%地貌縯變
요감%래주만%해안선%지모연변
remote sensing%Laizhou Bay%Coastline%Geomorphic evolution
以莱州湾东南岸1979~2014年的Landsat MSS/TM/OLI-TIRS影像为数据源,利用野外调查、遥感地貌解译和地理信息系统等方法,研究了近40年来莱州湾海岸地貌、海岸线和地貌淤蚀状态演变,分析了人类活动对地貌过程以及海岸线变迁的影响.结果表明:潍河河口、胶莱河河口、海庙港到刁龙嘴以及三山岛附近海岸岸线空间变化幅度较大,最大变化率为300.51 m/a,海岸淤涨明显,人工开发贡献较大;太平湾南端到海庙港以北海岸以及虎头崖西侧出现侵蚀.在人类活动影响下,自1979年以来,各地貌类型与盐田、养殖池之间的转化最为频繁、面积转化较大,海岸线向海推进明显,海岸开发到1988年进入一个围垦活跃期,之后围垦活动减弱,到2005年又进入一个小高峰,之后便进入平缓期.因此,最近40年来人类活动在莱州湾东南岸地貌演变过程中起着十分重要的作用,合理规划和规范开发活动是促进山东半岛蓝色经济区崛起的重要环节.
以萊州灣東南岸1979~2014年的Landsat MSS/TM/OLI-TIRS影像為數據源,利用野外調查、遙感地貌解譯和地理信息繫統等方法,研究瞭近40年來萊州灣海岸地貌、海岸線和地貌淤蝕狀態縯變,分析瞭人類活動對地貌過程以及海岸線變遷的影響.結果錶明:濰河河口、膠萊河河口、海廟港到刁龍嘴以及三山島附近海岸岸線空間變化幅度較大,最大變化率為300.51 m/a,海岸淤漲明顯,人工開髮貢獻較大;太平灣南耑到海廟港以北海岸以及虎頭崖西側齣現侵蝕.在人類活動影響下,自1979年以來,各地貌類型與鹽田、養殖池之間的轉化最為頻繁、麵積轉化較大,海岸線嚮海推進明顯,海岸開髮到1988年進入一箇圍墾活躍期,之後圍墾活動減弱,到2005年又進入一箇小高峰,之後便進入平緩期.因此,最近40年來人類活動在萊州灣東南岸地貌縯變過程中起著十分重要的作用,閤理規劃和規範開髮活動是促進山東半島藍色經濟區崛起的重要環節.
이래주만동남안1979~2014년적Landsat MSS/TM/OLI-TIRS영상위수거원,이용야외조사、요감지모해역화지리신식계통등방법,연구료근40년래래주만해안지모、해안선화지모어식상태연변,분석료인류활동대지모과정이급해안선변천적영향.결과표명:유하하구、효래하하구、해묘항도조룡취이급삼산도부근해안안선공간변화폭도교대,최대변화솔위300.51 m/a,해안어창명현,인공개발공헌교대;태평만남단도해묘항이북해안이급호두애서측출현침식.재인류활동영향하,자1979년이래,각지모류형여염전、양식지지간적전화최위빈번、면적전화교대,해안선향해추진명현,해안개발도1988년진입일개위은활약기,지후위은활동감약,도2005년우진입일개소고봉,지후편진입평완기.인차,최근40년래인류활동재래주만동남안지모연변과정중기착십분중요적작용,합리규화화규범개발활동시촉진산동반도람색경제구굴기적중요배절.
Taking the Landsat MSS/TM/OLI-TIRS remote sensing images since 1979 to 2014 as the main sources of information, field survey, remote sensing and GIS were used to study the change in coastal landforms,coastlines,geomorphic siltation and erosion patterns in southeastern of the Laizhou Bay for the last 40 years so as to trace the impact of human activities. The result shows that coastline at Weihe River,Jiaolai River,Haimiao Port,Diaolongzui,Sanshan Island changed largely,the maximum change rate was 300. 51 m/a, and the accretion was clear for the coast because of human activities;the erosion occurred at the south of Taip-ing Bay to the north of Haimiao Port and the west of Hutouya. As for effection of human,coastline advanced seaward gradually,the conversion was most frequently,and transformation of area was large,which showed dif-ferent landforms convert to salina and breeding pool since 1979 . The exploitation of coast became active in 1988 and 2005 then reached a plateau. Therefore,human activities played a very important role in the geomor-phologic process evolution of Laizhou Bay in recent 40 years. Hence, reasonable planning and specification de-velopment are important ways to promote the rise of Shandong Peninsula blue economic zone.