南方水产科学
南方水產科學
남방수산과학
SOUTH CHINA FISHERIES SCIENCE
2014年
3期
1-8
,共8页
罗昭林%朱长波%郭永坚%粟丽%李俊伟%区又君
囉昭林%硃長波%郭永堅%粟麗%李俊偉%區又君
라소림%주장파%곽영견%속려%리준위%구우군
流沙湾%沉积物%有机碳%氮%磷%污染评价
流沙灣%沉積物%有機碳%氮%燐%汙染評價
류사만%침적물%유궤탄%담%린%오염평개
Liusha Bay%sediment%organic carbon%nitrogen%phosphorus%pollution assessment
2012年5月至2013年1月,每季度在流沙湾内湾养殖区、外湾养殖区和外湾非养殖区采集沉积物和水质样品,测定沉积物的总有机碳(TOC)、总氮(TN)和总磷(TP)质量分数,以及底层水溶解氧(DO)和水温(T),结合水动力分析,研究其表层沉积物中富营养物质碳( C)、氮(N)、磷(P)的分布特征和受污染程度。结果表明,流沙湾的物理地形决定了湾内流场水流缓慢、内外湾之间水交换过程缓慢的固有特征。底层水 DO 自春季开始逐步升高,冬季达到最大值。内湾养殖区的底层水 DO 均值低于外湾。表层沉积物 TOC 和 TP 质量分数没有明显的季节差异,但 TN 质量分数在春、夏季明显高于秋、冬季。养殖区的 TOC、TN 质量分数均显著高于非养殖区,且以内湾养殖区最高,其 TP 空间差异不显著。流沙湾表层沉积物 TOC 年平均有机碳污染指数为1.29,TN污染指数达2.98,而 TP 磷污染指数仅为0.92,表明该海域已受到中等水平的氮污染和低水平的有机碳污染,且现有养殖格局加速了养殖区的富营养物质沉积。
2012年5月至2013年1月,每季度在流沙灣內灣養殖區、外灣養殖區和外灣非養殖區採集沉積物和水質樣品,測定沉積物的總有機碳(TOC)、總氮(TN)和總燐(TP)質量分數,以及底層水溶解氧(DO)和水溫(T),結閤水動力分析,研究其錶層沉積物中富營養物質碳( C)、氮(N)、燐(P)的分佈特徵和受汙染程度。結果錶明,流沙灣的物理地形決定瞭灣內流場水流緩慢、內外灣之間水交換過程緩慢的固有特徵。底層水 DO 自春季開始逐步升高,鼕季達到最大值。內灣養殖區的底層水 DO 均值低于外灣。錶層沉積物 TOC 和 TP 質量分數沒有明顯的季節差異,但 TN 質量分數在春、夏季明顯高于鞦、鼕季。養殖區的 TOC、TN 質量分數均顯著高于非養殖區,且以內灣養殖區最高,其 TP 空間差異不顯著。流沙灣錶層沉積物 TOC 年平均有機碳汙染指數為1.29,TN汙染指數達2.98,而 TP 燐汙染指數僅為0.92,錶明該海域已受到中等水平的氮汙染和低水平的有機碳汙染,且現有養殖格跼加速瞭養殖區的富營養物質沉積。
2012년5월지2013년1월,매계도재류사만내만양식구、외만양식구화외만비양식구채집침적물화수질양품,측정침적물적총유궤탄(TOC)、총담(TN)화총린(TP)질량분수,이급저층수용해양(DO)화수온(T),결합수동력분석,연구기표층침적물중부영양물질탄( C)、담(N)、린(P)적분포특정화수오염정도。결과표명,류사만적물리지형결정료만내류장수류완만、내외만지간수교환과정완만적고유특정。저층수 DO 자춘계개시축보승고,동계체도최대치。내만양식구적저층수 DO 균치저우외만。표층침적물 TOC 화 TP 질량분수몰유명현적계절차이,단 TN 질량분수재춘、하계명현고우추、동계。양식구적 TOC、TN 질량분수균현저고우비양식구,차이내만양식구최고,기 TP 공간차이불현저。류사만표층침적물 TOC 년평균유궤탄오염지수위1.29,TN오염지수체2.98,이 TP 린오염지수부위0.92,표명해해역이수도중등수평적담오염화저수평적유궤탄오염,차현유양식격국가속료양식구적부영양물질침적。
We collected the sediment and water samples from breeding areas,farming areas and non-farming areas outside Liusha Bay quar-terly during May,2012 to January,2013,and determined the total organic carbon(TOC),total nitrogen(TN)and total phosphorus(TP) content in the sediment,as well as dissolved oxygen(DO)and temperature(T)in the bottom water,hydrodynamically analyzing the distri-bution characteristics of C,N,P and their pollution. The results indicate that the physical terrain of Liusha Bay determined the slow flow of water inside the bay and the slow water exchange between inner and outer parts of the bay. The DO in bottom water significantly rose from spring to winter and reached the maximum. The DO in bottom water in inner bay was lower than that in outer bay. The TOC and TP contents in surface sediment had no significant seasonal changes,but the TN contents in spring and summer were obviously higher than those in au-tumn and winter. The TOC and TN contents in the sediment of the breeding areas were significantly higher than those in the non-breeding ar-ea,being the highest in the inner bay. The TP content showed no significant time and spatial difference. The annual average pollution indi-ces for TOC,TN and TP were 1. 29,2. 98 and 0. 92,respectively,which indicated that the bay had suffered medium organic carbon pollu-tion and low nitrogen pollution,and current aquaculture status had significantly accelerated eutrophic sedimentation in Liusha Bay.