2017
DOI: 10.1007/s13131-017-1042-y
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The evolution characteristics of main waterways and their control mechanism in the radial sand ridges of the southern Yellow Sea

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Cited by 12 publications
(7 citation statements)
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“…One of the geomorphologically amazing (Chen et al 2017), globally unique, yet ecologically very poorly studied coastal areas in China, is the complex of intertidal habitats along the Dafeng-Dongtai-Rudong coastline in southern Jiangsu Province, a complex that includes the Tiaozini mudflats along the mainland coast and the offshore Dongsha Shoals (32.4-33.4°N, 120.7-121.5°E;Kang et al 2017;Xiong et al 2017, see Fig. 3).…”
Section: ) Is Includes Coastal Areas Being Designated Asmentioning
confidence: 99%
“…One of the geomorphologically amazing (Chen et al 2017), globally unique, yet ecologically very poorly studied coastal areas in China, is the complex of intertidal habitats along the Dafeng-Dongtai-Rudong coastline in southern Jiangsu Province, a complex that includes the Tiaozini mudflats along the mainland coast and the offshore Dongsha Shoals (32.4-33.4°N, 120.7-121.5°E;Kang et al 2017;Xiong et al 2017, see Fig. 3).…”
Section: ) Is Includes Coastal Areas Being Designated Asmentioning
confidence: 99%
“…However, this steepening of the mudflat is also observed at similar mudflats along the Jiangsu coast, which is driven by (longshore) tidal currents [59,93]. Additionally, the Yaosha shoal-channel system indeed migrates southward [94] (similar to other channel-shoal systems along the Jiangsu coast [95,96]). The siltation at the center of Yaosha can also be seen in the increase of supralittoral at the center of Yaosha (Figure 10b).…”
Section: Alternative Port Configurationsmentioning
confidence: 79%
“…When the ratio is greater than 1, Ca 2+ and SO 4 2− in groundwater mainly come from the dissolution of calcite or dolomite. In Figure 4d, the Taihui water samples after grouting are distributed below the 1:1 line, indicating that in addition to the dissolution of gypsum, SO 4 2− has other sources, such as the oxidation of pyrite [45,46]. According to the borehole histogram of the study area, pyrite exists in the limestone fissures of C 3 II and C 3 III groups.…”
Section: Ion Combination Ratiomentioning
confidence: 94%