海洋通报
海洋通報
해양통보
MARINE SCIENCE BULLETIN
2014年
5期
559-565
,共7页
王小丹%方成%康慧%谢海澜%柳富田%孟琳
王小丹%方成%康慧%謝海瀾%柳富田%孟琳
왕소단%방성%강혜%사해란%류부전%맹림
潮间带%潮滩%曹妃甸%遥感%演变监测
潮間帶%潮灘%曹妃甸%遙感%縯變鑑測
조간대%조탄%조비전%요감%연변감측
tidal zone%tidal flat%Caofeidian%remote sensing%evolution monitoring
选用美国Landsat系列卫星、中巴卫星CBERS及中国HJ-1卫星1981-2011年7个时相的遥感数据及潮汐潮位资料,应用“相同潮位对比法”,分析研究了曹妃甸地区潮间带的空间分布特征和潮滩动态演变趋势。结果表明:近三十年来,受潮滩围垦、填海造陆等人类活动的影响,潮间带形态发生了很大变化,潮间带上边界逐渐向海推进,最大推进距离达3 km左右,使得上部潮滩面积不断减少;同时,受输沙量减少、风浪冲刷、沉降作用及海平面上升等因素的综合影响,潮滩下部整体上处于侵蚀状态,西部滩面侵蚀较轻,东部滩面侵蚀较严重。另外,在该区大规模开发建设期间,潮滩的平衡状态被破坏,部分岸段出现了潮滩暂时淤高的现象。
選用美國Landsat繫列衛星、中巴衛星CBERS及中國HJ-1衛星1981-2011年7箇時相的遙感數據及潮汐潮位資料,應用“相同潮位對比法”,分析研究瞭曹妃甸地區潮間帶的空間分佈特徵和潮灘動態縯變趨勢。結果錶明:近三十年來,受潮灘圍墾、填海造陸等人類活動的影響,潮間帶形態髮生瞭很大變化,潮間帶上邊界逐漸嚮海推進,最大推進距離達3 km左右,使得上部潮灘麵積不斷減少;同時,受輸沙量減少、風浪遲刷、沉降作用及海平麵上升等因素的綜閤影響,潮灘下部整體上處于侵蝕狀態,西部灘麵侵蝕較輕,東部灘麵侵蝕較嚴重。另外,在該區大規模開髮建設期間,潮灘的平衡狀態被破壞,部分岸段齣現瞭潮灘暫時淤高的現象。
선용미국Landsat계렬위성、중파위성CBERS급중국HJ-1위성1981-2011년7개시상적요감수거급조석조위자료,응용“상동조위대비법”,분석연구료조비전지구조간대적공간분포특정화조탄동태연변추세。결과표명:근삼십년래,수조탄위은、전해조륙등인류활동적영향,조간대형태발생료흔대변화,조간대상변계축점향해추진,최대추진거리체3 km좌우,사득상부조탄면적불단감소;동시,수수사량감소、풍랑충쇄、침강작용급해평면상승등인소적종합영향,조탄하부정체상처우침식상태,서부탄면침식교경,동부탄면침식교엄중。령외,재해구대규모개발건설기간,조탄적평형상태피파배,부분안단출현료조탄잠시어고적현상。
By choosing seven scenes' remote sensing data of American Landsat and CBERS, HJ-1 from 1981 to 2011 and tide and sea level data, and applying the method of “same sea level contrasting” , the paper analyzed and studied the spatial distribution of tidal zone and the dynamic evolution trend of tidal flat in Caofeidian. The results indicated that in the past thirty years, shape of tidal zone had changed greatly because it was affected by human activities such as the tidal flat reclamation and sea reclamation. The upper bound of tidal zone advanced seaward gradually with about 3 km of maximum distance, which made the upper part of tidal flat area reduced constantly. Meanwhile, affected by the sediment runoff decrease, storm washing, subsidence and sea level rise, the lower part of tidal flat was eroded overall, and the west part was gentle, and the east part was more severe. In addition, the balance of tidal flat was broken during the large-scale exploitation and construction in this area, and the tidal flat deposited temporarily in some coasts.