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印度东海岸卡尔帕卡姆沿海海域理化性质的季节性变化,特别强调营养物质。

Seasonal variation in physicochemical properties of coastal waters of Kalpakkam, east coast of India with special emphasis on nutrients.

机构信息

Environmental & Industrial Safety Section, Indira Gandhi Center for Atomic Research, Kalpakkam, 603 102, Tamil Nadu, India.

出版信息

Environ Monit Assess. 2010 May;164(1-4):153-71. doi: 10.1007/s10661-009-0882-0. Epub 2009 Apr 29.

Abstract

A study pertaining to the seasonal variation in physicochemical properties of the coastal waters was carried out at Kalpakkam coast for a period of 1 year (February 2006 to January 2007). It revealed that the coastal water was significantly influenced by freshwater input during North East (NE) monsoon and post-monsoon periods. Concentration of all the nutrients and dissolved oxygen (DO) was relatively high during the NE monsoon, whereas, salinity and chlorophyll-a (chl-a) were at their minimum level during this period. Phytoplankton production peak was observed in summer during which a typical marine condition prevailed. The present observed values of nitrate, phosphate, silicate, and turbidity are significantly high (five to ten times) compared to that of the pre-Tsunami period from this coast. Relatively low DO and chl-a concentration was noticed during the post-Tsunami period. A notable feature of this study is that though nutrient concentration in the coastal waters during post-Tsunami period has increased significantly, turbidity, the most single dominating factor, was found to adversely affect the phytoplankton production during post-Tsunami period as reflected by relatively low chl-a concentration. Thus, the post-Tsunami period may result in a change in coastal biodiversity pattern concomitant with change in coastal water quality.

摘要

一项关于沿海海域理化性质季节性变化的研究在卡尔帕卡姆海岸进行了为期一年(2006 年 2 月至 2007 年 1 月)。结果表明,在东北季风和季风后期间,沿海水受到淡水输入的显著影响。在东北季风期间,所有营养物质和溶解氧(DO)的浓度相对较高,而盐度和叶绿素-a(chl-a)在这期间处于最低水平。浮游植物产量峰值出现在夏季,期间出现典型的海洋状况。与海啸前时期相比,目前从该海岸观察到的硝酸盐、磷酸盐、硅酸盐和浊度值显著升高(五到十倍)。海啸后期间,注意到相对较低的 DO 和 chl-a 浓度。本研究的一个显著特点是,尽管海啸后期间沿海水域的营养物质浓度显著增加,但浊度是最单一的主导因素,被发现对海啸后期间的浮游植物产量产生不利影响,反映为相对较低的 chl-a 浓度。因此,海啸后期间可能会导致沿海生物多样性模式发生变化,同时沿海水质也会发生变化。

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