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首页> 外文期刊>Fresenius environmental bulletin >NUTRIENT EXCRETION BY Limnodrilus hoffmeisteri Claparède IN LAKE TAIHU, A LARGE, SHALLOW LAKE OF CHINA
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NUTRIENT EXCRETION BY Limnodrilus hoffmeisteri Claparède IN LAKE TAIHU, A LARGE, SHALLOW LAKE OF CHINA

机译:大型浅水湖泊太湖中的Limnodrilus hoffmeisteriClaparède对营养的排泄

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To study the potential significance of Limnodrilus hoffmeisteri, a dominant benthic organism in Lake Taihu, on lake eutrophication, the effect of temperature and density on the ammonium (NH4+-N) and phosphate (PO43--P) excretion rates of L. hoffmeisteri was performed. Using a regression equation describing the relationship between temperature and the NH4+-N and PO43--P excretion rates of L. hoffmeisteri while considering water temperature and L. hoffmeisteri biomass in Taihu between 2007–2010, we estimated the potential nitrogen and phosphorus contribution of L. hoffmeisteri to Lake Taihu. With increasing temperature, both the NH4+-N and PO43--P excretion rates of L. hoffmeisteri gradually increased while changes in density did not significantly affect the excretion rate of NH4+-N and PO43--P. The annual average NH4+-N and PO43--P excretion by L. hoffmeisteri were 1925.54 and 210.0 t, respectively. These amounts were up to 19.3 and 23.3% of the annual NH4+-N and PO43--P net flux of the entire sedimentwater interface in Lake Taihu, and are only less than the two primary exogenous nutrient sources—indirect lakeside and watercourse nitrogen and phosphorus inputs. This study showed that nutrient excretion of L. hoffmeisteri has a significant effect on eutrophication in Lake Taihu.
机译:为了研究太湖的主要底栖生物Limnodrilus hoffmeisteri对富营养化的潜在意义,温度和密度对Loff hoffmeisteri铵(NH4 + -N)和磷酸盐(PO43--P)排泄率的影响执行。使用回归方程描述温度与太湖乳酸菌NH4 + -N和PO43-P排泄率之间的关系,同时考虑2007-2010年太湖的水温和霍夫迈斯特氏菌生物量,我们估算了太湖的氮和磷的潜在贡献L. hoffmeisteri到太湖。随着温度的升高,霍夫曼氏乳杆菌的NH4 + -N和PO43-P排泄率逐渐增加,而密度的变化并没有显着影响NH4 + -N和PO43-P的排泄率。霍夫迈斯特氏菌的年平均NH4 + -N和PO43-P排泄分别为1925.54和210.0 t。这些量分别占太湖整个沉积水界面的年度NH4 + -N和PO43-P净通量的19.3%和23.3%,仅小于两个主要的外源养分来源-间接湖边和河道氮和磷输入。这项研究表明,霍夫迈斯特氏菌的养分排泄对太湖的富营养化具有显着影响。

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