The spatial distribution, present status, and evolution rules of seabed villages ruins in Hainan Dongzhai Port were studied based on space archaeology by using high-precision UAV (unmanned aerial vehicles) orthophoto images, digital elevation model (DEM), Landsat8 images, and field surveys. The results are showed as follows. Firstly, the seabed villages ruins are evenly distributed on both sides of the ancient channel of Dongzhai River. Secondly, some of the seabed villages ruins sink below the sea surface, and some of them are partially exposed after the tide ebbs because these ruins are located in the forefront area of the land-sea interaction, where the geological conditions are unstable. Thirdly, the seabed villages ruins near Linshi Village will continue to sink due to the influence of the earthquake events. The middle part of the ruins have been washed away by the tidal fluctuations, and that part covers an area of about 1 871.5 m2 which accounts for 31.5% of the total area of the ruins. Overall, this study is important for the seabed villages ruins protection in Dongzhai Port and also has significance for the development of the Maritime Silk Road.
LI Zhixin
,
WANG Xinyuan
,
LIU Chuansheng
,
LUO Lei
. Remote sensing observation and analysis of seabed villages ruins in Dongzhai Port in Hainan Island[J]. Journal of University of Chinese Academy of Sciences, 2019
, 36(6)
: 803
-809
.
DOI: 10.7523/j.issn.2095-6134.2019.06.011
[1] 徐起浩. 对雷琼凹陷地震地质的认识[J]. 华南地震, 1986(1):86-96.
[2] 陈恩民, 黄咏茵. 1605年海南岛琼州大地震及其发震构造的初步探讨[J]. 地震地质, 1979(4):39-46,101-102.
[3] 黄咏茵, 陈恩民, 苏丹. 1605年琼州大地震震源区区域重、磁场特征及深部构造背景研究(Ⅱ)(续)[J]. 华南地震, 1988(3):5-27.
[4] 张虎男, 赵希涛. 雷琼地区新构造运动的特征[J]. 地质科学, 1984(3):276-287.
[5] 徐起浩. 1605年琼州大地震陆陷成海和可能的海啸[J]. 海洋学报(中文版), 2007, 29(3):146-156.
[6] 张汉女. 地理信息系统支持下的福建省水下考古研究[D]. 长春:吉林大学, 2013.
[7] 王心源, 陆应诚, 高超,等. 广义遥感环境考古的技术整合[J]. 安徽大学学报(自然科学版), 2005, 29(2):40-44.
[8] Giardino M J. A history of NASA remote sensing contributions to archaeology[J]. Journal of Archaeological Science, 2011, 38(9):2 003-2 009.
[9] Lasaponara R, Masini N. Satellite remote sensing:a new tool for archaeology[J]. Journal of Archaeological Science, 2013, 40(10):3 672-3 673.
[10] 王心源, 吴立, 吴学泽,等. 巢湖凌家滩遗址古人类活动的地理环境特征[J]. 地理研究, 2009, 28(5):1 208-1 216.
[11] Luo L, Wang X, Liu C, et al. Integrated RS, GIS and GPS approaches to archaeological prospecting in the Hexi Corridor, NW China:a case study of the royal road to ancient Dunhuang[J]. Journal of Archaeological Science, 2014, 50(1):178-190.
[12] 公雪霜, 于丽君, 聂跃平,等. 辽宁西部地区先秦时期聚落遗址空间格局分析[J]. 中国科学院大学学报, 2016, 33(3):373-379.
[13] 王心源, 郭华东. 空间考古学:对象、性质、方法及任务[J]. 中国科学院院刊, 2015(3):360-367.
[14] Guo H. Steps to the digital Silk Road[J]. Nature, 2018, 554(7 690):25-27.
[15] 王荣丽, 管伟, 邱明红,等. 东寨港红树林退化动态初步分析[J]. 中南林业科技大学学报, 2017, 37(2):63-68.
[16] 徐起浩. 琼北东寨港地区的近期下沉[J]. 海洋科学, 1986, 10(1):24-28.
[17] 徐起浩. 海南岛北部东寨港的形成、变迁与1605年琼州大地震[J]. 地震地质, 1986(3):94-98.
[18] 赵英时. 遥感应用分析原理与方法[M]. 北京:科学出版社, 2003.
[19] 刘亮, 姜小光, 刘善伟,等. WorldView-2影像的水深探测能力[J]. 中国科学院大学学报, 2017,34(1):64-68.
[20] 吴爱琴, 赵红杰, 杨瑞霞,等. 开封市古城址和古河道遥感考古试验研究[J]. 地域研究与开发, 2002, 21(3):85-88.
[21] 张家声, 高祥林, 黄雄南. 亚洲中部地震构造解析[M]. 北京:地震出版社, 2014.
[22] 丁莹莹, 赵希涛, 胡道功,等. 琼东北晚新生代断裂活动及其对东寨港沉降的控制作用[J]. 地球学报,2018,39(2):155-166.
