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莱州湾东岸动力地貌对陆海相互作用的响应研究

杜国云

海洋科学2016,Vol.40Issue(8):70-75,6.
海洋科学2016,Vol.40Issue(8):70-75,6.DOI:10.11759/hykx/20141209

莱州湾东岸动力地貌对陆海相互作用的响应研究

Dynamic geomorphological response to land-sea interaction on the eastern coast, Laizhou Bay

杜国云1

作者信息

  • 1. 鲁东大学资源与环境工程学院,山东烟台 264025
  • 折叠

摘要

Abstract

Based on SRTM3_DEM and RS analyses, field survey data and previous studies, this study examines the geomorphic features and landform growth of the coastal alluvial marine plain on the east coast of Laizhou Bay. The results show that the geomorphologic structure of the coast occurs as a barrier-lagoon system in the transverse di-rection and a tombolo-lagoon system in the longitudinal direction. Systematic bending characteristics occur in the downstream channels of the rivers as they enter the sea, which correspond with the barrier-lagoon system. This is the most significant sign of fluvial geomorphological response to coastal land-ocean interaction since the mid-Holocene. Hydrologic analysis of the DEM shows that the terrain inclines in two directions, from east to west and south to north, and the watershed extraction from the Wanghe river corresponds to the watershed extraction downstream of the Wanghe paleochannel from east to west. This results in the expression of the current channel and paleochannel manifesting by different threshold values.

关键词

DEM/河流地貌/沙坝-潟湖系统/全新世/莱州湾

Key words

DEM/river geomorphology/barrier-lagoon system/Holocene/Laizhou Bay

分类

天文与地球科学

引用本文复制引用

杜国云..莱州湾东岸动力地貌对陆海相互作用的响应研究[J].海洋科学,2016,40(8):70-75,6.

基金项目

山东省自然科学基金资助项目(ZR2013DL006)@@@@Natural Science Foundation of Shandong Province, No. ZR2013DL006。 (ZR2013DL006)

海洋科学

OA北大核心CSCDCSTPCD

1000-3096

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