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Effects of the anthropogenic activities on the morphological evolution of the Modaomen Estuary,Pearl River Delta,China 总被引：1，自引：0，他引：1
Owing to the intensive human activities, the Modaomen Estuary has been significantly modified since 1950s, which has resulted in considerable changes of hydrodynamics and morphodynamics in the area. In this paper, the effects of the anthropogenic activities on the hydrodynamics and morphological evolution in the estuary at different stages are systematically assessed based on the detailed bathymetric data and field survey. The results show that the human activities have caused the channelization of the enclosed sea area in the Modamen Estuary;fast seaward movement of the mouth bar with high siltation;expansion of the channel volume due to channel deepening. The paper also highlights the main hydrodynamic changes in the estuary, including the rise of the water level;the distinguishing changes of tidal range before and after the 1990s （decrease and increase respectively）; as well as the increase of the divided flow ratio. It is found that reclamation is the main factor promoting the transition of nature of the estuary from runoff dominant to runoff and wave dominant, and sand mining activities are mainly to strengthen the tidal dynamic and to low the water level. The results provide useful guidance for better planning of the future developments in the estuary and further research in the area. 相似文献
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Owing to the intensive human activities, the Modaomen Estuary has been significantly modified since 1950s, which has resulted in considerable changes of hydrodynamics and morphodynamics in the area. In this paper, the effects of the anthropogenic activities on the hydrodynamics and morphological evolution in the estuary at different stages are systematically assessed based on the detailed bathymetric data and field survey. The results show that the human activities have caused the channelization of the enclosed sea area in the Modamen Estuary; fast seaward movement of the mouth bar with high siltation; expansion of the channel volume due to channel deepening. The paper also highlights the main hydrodynamic changes in the estuary, including the rise of the water level; the distinguishing changes of tidal range before and after the 1990s (decrease and increase respectively); as well as the increase of the divided flow ratio. It is found that reclamation is the main factor promoting the transition of nature of the estuary from runoff dominant to runoff and wave dominant, and sand mining activities are mainly to strengthen the tidal dynamic and to low the water level. The results provide useful guidance for better planning of the future developments in the estuary and further research in the area. 相似文献
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针对城市犯罪分布环境的研究问题,本文基于兰州市的犯罪统计数据,结合POI大数据,使用空间统计和GIS空间分析方法提取了兰州市3种类型犯罪的热点区,并进一步使用POI数据探索了犯罪热点区内的环境特征。结果表明:1)兰州市4个城区内犯罪分布情况不同,主要集中在人口较多的黄河南岸,其中又以西站、西湖公园、"西关十字—南关十字"一线、西固城步行街等区域为主,城关区作为中心城区,犯罪行为分布范围广,犯罪高发区多。2) 3类犯罪热点区的设施点环境多数是多类型POI设施共同主导,少数是单类型POI设施主导,但起主导作用的POI类型都能反映出对应的主要犯罪类型对城市环境的要求特点。3) 3类犯罪对人流、财富以及场所隐蔽性的趋向性不同,并在对应环境的POI分布特征中得到体现。 相似文献
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The delta evolution and erosion process of the abandoned Yellow River Delta(AYRD) have been extensively studied. However, the variation of sediment at a large littoral scale along the north coast of Jiangsu is less understood. In this study, the data of surface sediment samples obtained in the littoral area of the Yellow River Delta in 2006 and 2012 is used to study the sediment variability and sediment transport trends by using the geostatistics analysis tool and the grain size trend analysis model. In order to ensure the applicability of the model, the geostatistics method is used to determine the characteristic distance(Dc) with the average range value(Ao) of grain size parameter. Filtering method(removing data that not at a sampling station) is used to improve accuracy of data selection. The results show that sedimentary spatial correlation in Lianyun Port area and southern part of the abandoned Yellow River Delta(AS) is better than that in the northern part of the abandoned Yellow River Delta(AN). Sediment in the area is found to be anisotropy at the northeast–southeast direction. The grain size trend analysis reveals that the sediment trend is towards bayhead and southerly in the Haizhou Bay, southeasterly along the shoreline in the south Lianyun Port, northwesterly in AN and easterly–southeasterly in AS respectively. The investigation of possible relationships between Dc, Ao, sediment transport and delta evolution shows a close link between Dc and Ao of one sediment combination. It is also found that sediment transport trends could reasonably represent the delta evolution to a certain degree. 相似文献
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