热带海洋学报
熱帶海洋學報
열대해양학보
JOURNAL OF TROPICAL OCEANOGRAPHY
2014年
4期
77-84
,共8页
程香菊%郭振仁%刘国%李兵
程香菊%郭振仁%劉國%李兵
정향국%곽진인%류국%리병
大亚湾水产养殖区%沉积物-水界面%氮磷%扩散
大亞灣水產養殖區%沉積物-水界麵%氮燐%擴散
대아만수산양식구%침적물-수계면%담린%확산
aquaculture region of Daya bay%sediment-water interface%nitrogen and phosphorus%diffusion
为了更好地跟踪水产养殖活动对海湾水环境的影响,于2011年10月采集了3个具有代表性的大亚湾海域水产养殖区的水样和底泥样品,研究了底泥含水率、孔隙率、密度以及孔隙水中的氨氮和可溶活性磷酸盐的垂直分布。采用经典的Fick定律,计算了氮和磷在沉积物-水界面的释放速率和年释放量。基于环境水力学理论,应用水平二维数学模型,计算了氮和磷在沉积物-水界面释放之后在海水中的扩散迁移时空分布。结果表明,澳头、深水港、虎头门采样点沉积物-水界面的氨氮年释放量分别为13.5、5.2、0.56t·a-1,可溶活性磷酸盐的释放量分别为0.34、0.03、0.02t·a-1,使水产养殖区域沉积物成为极具潜力的污染内源。释放到海水中的氮和磷受潮流、风、水深的影响,其扩散迁移范围呈长条形带状分布。每个养殖区域的污染带长度约为1km,横向宽度约为50m。该区域的海水极易呈富营养化状态。
為瞭更好地跟蹤水產養殖活動對海灣水環境的影響,于2011年10月採集瞭3箇具有代錶性的大亞灣海域水產養殖區的水樣和底泥樣品,研究瞭底泥含水率、孔隙率、密度以及孔隙水中的氨氮和可溶活性燐痠鹽的垂直分佈。採用經典的Fick定律,計算瞭氮和燐在沉積物-水界麵的釋放速率和年釋放量。基于環境水力學理論,應用水平二維數學模型,計算瞭氮和燐在沉積物-水界麵釋放之後在海水中的擴散遷移時空分佈。結果錶明,澳頭、深水港、虎頭門採樣點沉積物-水界麵的氨氮年釋放量分彆為13.5、5.2、0.56t·a-1,可溶活性燐痠鹽的釋放量分彆為0.34、0.03、0.02t·a-1,使水產養殖區域沉積物成為極具潛力的汙染內源。釋放到海水中的氮和燐受潮流、風、水深的影響,其擴散遷移範圍呈長條形帶狀分佈。每箇養殖區域的汙染帶長度約為1km,橫嚮寬度約為50m。該區域的海水極易呈富營養化狀態。
위료경호지근종수산양식활동대해만수배경적영향,우2011년10월채집료3개구유대표성적대아만해역수산양식구적수양화저니양품,연구료저니함수솔、공극솔、밀도이급공극수중적안담화가용활성린산염적수직분포。채용경전적Fick정률,계산료담화린재침적물-수계면적석방속솔화년석방량。기우배경수역학이론,응용수평이유수학모형,계산료담화린재침적물-수계면석방지후재해수중적확산천이시공분포。결과표명,오두、심수항、호두문채양점침적물-수계면적안담년석방량분별위13.5、5.2、0.56t·a-1,가용활성린산염적석방량분별위0.34、0.03、0.02t·a-1,사수산양식구역침적물성위겁구잠력적오염내원。석방도해수중적담화린수조류、풍、수심적영향,기확산천이범위정장조형대상분포。매개양식구역적오염대장도약위1km,횡향관도약위50m。해구역적해수겁역정부영양화상태。
In order to better track the effect of marine culture in floating cage on water quality, the sediments of three representative sites in the aquaculture area of Daya Bay were sampled in October 2011. The water percentage, porosity percentage and density of sediments, and the vertical distributions of nitrogen and phosphorus in the interstitial water were measured in laboratory experiments. The release rate and yearly release quantity of nutrients at the sediment-water interface were calculated by means of Fick’s Law. Based on the theory of environmental hydraulics, a two-dimensional numerical model was applied to calculate diffusion regularities of the nutrients. The results show that, the yearly release contents of ammonia across the interface of sediment-water at Aotou, Shenshuigang and Hutoumen were 13.5, 5.2, 0.56 t·a-1, and that of dissolved reactive phosphorus were 0.34, 0.03, 0.02 t·a-1, respectively. The release fluxes were high enough to make the sediments close to the aquaculture area become a potential pollution source. The released nutrients from the sediment-water interface were affected by tidal flow, wind, and depth, and the diffusion region in seawater had a strip shape. The pollution belt was about 1 km in length and 50 m in width at each sampled site of the aquaculture area, which made eutrophication a potential risk to the water body.