the changjiang estuary region 长江河口地区
the changjiang estuary mud area 长江口泥质区
the Changjiang Yangtze River estuary 长江口
the changjiang river estuary 长江河口
the Changjiang River and estuary 长江流域及长江口
The pH range within the Changjiang estuary is limited to 7.7-8.3.
长江口水体pH的变化范围基本为7.7-8.3。
参考来源 - 长江口悬浮泥沙的吸附—解吸作用对元素固—液相态转化控制的研究The Changjiang Estuary serves as an important land-ocean interaction region and can be taken as a natural laboratory for studying estuarine biogeochemical processes.
长江河口区是研究陆-海相互作用的重要场所，可作为研究生物地球化学过程的天然实验室。
参考来源 - 长江口悬浮泥沙的吸附—解吸作用对元素固—液相态转化控制的研究·2,447,543篇论文数据，部分数据来源于NoteExpress
The Changjiang estuary is divided into south and north branches by the Chongming Island.
长江口被崇明岛分为南北两支。
The islands in the Changjiang estuary, such as Chongming, Changxing and Hengsha, are originally of Holocene river-mouth bars.
长江口崇明、长兴、横沙等岛屿是由全新世长江的河口沙坝孕育而成。
The South Passage which is little affects by the human being is the main channel of water discharge and sediment in the Changjiang Estuary.
南槽是长江口主要的水沙交换通道之一，受人类活动影响较小。
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