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2004年夏季太湖梅梁湾席状漂浮水华风力漂移入湾量计算
摘要点击 2231  全文点击 2240  投稿时间:2004-11-06  修订日期:2005-01-06
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中文关键词  太湖梅梁湾  席状水华  风力漂移  漂移速度  风速
英文关键词  Meiliang Bay of Taihu Lake  floating mat-like algal bloom  wind-driven algae drift  algae drift velocity  wind speed
作者单位
白晓华 中国科学院南京地理与湖泊研究所,南京210008 
胡维平 中国科学院南京地理与湖泊研究所,南京210008 
胡志新 中国科学院南京地理与湖泊研究所,南京210008 
李香华 中国科学院南京地理与湖泊研究所,南京210008 
中文摘要
      太湖北部重度水华暴发时,在夏季盛行风推动下,漂浮的席状水华可由大太湖漂移进入位于太湖北部的梅梁湾,使湾内的水华加剧.本文通过室内风箱水槽实验和野外观测,对水华的风力漂移作了定量研究,建立了风速与水华漂移速度的指数相关方程.并据此对2004年夏季太湖北部发生席状水华的6d分别计算了水华风力漂移入湾量.6d中,只有2004-07-31水华漂移是由湾内向大太湖输出,且量很小,只有0.05 km2;其余5d水华漂移进入梅梁湾的面积占整个梅梁湾面积的3.7%~13.3%,进入量最大的是2004-06-11,达17.4km2,最少的是2004-07-30,为4.8 km2.
英文摘要
      Driven by the prevailing south wind in summer,floating mat-like algal blooms in the open area of Taihu Lake would drift into Meiliang Bay located in the northern part of Taihu Lake.An exponential relationship between wind speed and algal drift velocity was found through controlled flume experiments and field observations.Then the relationship was applied to compute drift importation into Meiliang Bay in six dates when mat-like algal blooms were happening.During the six dates,except on 2004-07-31 the algal boom drifted outwards from Meiliang Bay with slight amounts of 0.05km2;for the rest of dates,the importations were inwards positive,the maximum importation occurred on 2004-06-11,being 17.4km2,and the minimum importation on 2004-07-30,being 4.8km2;The results indicated importation of wind-driven algae drift during 24 hours accounts for 3.7%~13.3% of the area of Meiliang Bay.

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