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Tempora卜spatial Change of Cr Content in Bottom Waters
  • 时间:0
  • 分类:P[天文地球]
  • 作者机构:[1]Karst Wetland Ecology Research Center, Guizhou Minzu University, Guiyang 550025, China, [2]School of Chemistry and Environmental Sciences,Guizhou Minzu University, Guiyang 550025, China, [3]North China Sea Environmental Monitoring Center, State Oceanic Administration,Qingdao 266033, China
  • 相关基金:Supported by the China National Natural Science Foundation(31560107) ; Doctoral Degree Construction Library of Guizhou MinzuUniversity, Education Ministry's New Century Excellent Talents SupportingPlan ( NCET-12-0659) ; Innovation Group Major Program ofGuizhou Province (KY[2013]405, KY[2016]029) ; Research Projectsof Guizhou Province Ministry of Science and Technology (LH [2014]7376) ; Research Projects of Guizhou Minzu University ([201 4] 02) ;Research Projects of Guizhou Province Ministry of Education ( KY[2014]266).
中文摘要:

Based on the investigation data of Jiaozhou Bay waters in 1981, current situation and horizontal distribution of Cr content in bottom waters of Jiaozhou Bay mouth were studied. Results showed that in bottom waters of Jiaozhou Bay center, Cr content changed from 0. 50 to 3.78 mQ/L in April. In August, Cr content changed from 0.14 to 1.42 ng/L in bottom waters of Jiaozhou Bay mouth. It showed that Cr content corresponded with national class-one seawater quality standard (50.00 mQ/L) at different times and spaces, and Cr content was far less than 5.00 Therefore, under the effect of vertical water body, water quality was clean in bottom waters of Jiaozhou Bay, which was not polluted by Cr. In bottom waters of Jiaozhou Bay center in April and bottom waters of Jiaozhou Bay mouth in August, Cr transported by the river came to the bottom layer from surface layer by passing through water body in temporal-spatial change process. Under the effects of gravity and water flow, Cr continuously and quickly sank to the sea bottom. It verified the sedimentation process of Cr content.

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