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首页> 外文期刊>Fresenius Environmental Bulletin >PHOSPHORUS FRACTIONS IN SEDIMENT PROFILES OF THE EUTROPHIC LAKE MOGAN, TURKEY
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PHOSPHORUS FRACTIONS IN SEDIMENT PROFILES OF THE EUTROPHIC LAKE MOGAN, TURKEY

机译:土耳其富营养莫根湖沉积物剖面中的磷组分

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This study was conducted between July 2004 and June 2005 to determine the seasonal and spatial patterns of phosphorus in the littoral sediment of Lake Mogan, and its potential release into the lake water. Total phosphorus and phosphorus fractions in the sediment and overlying water samples were taken mainly from a selected station in the lake, and additionally, some chemical and physical parameters were measured. The amount of released phosphorus was estimated using the total filterable orthophosphate concentrations related to the sediment pore as well as overlying waters with the water content of the sediment, and the diffusion coefficient depending on the temperature. During the research period, sediment phosphorus release fluctuated between 0.002-0.062 μg.m~(-2)d~(-1) reaching a minimum in November and a maximum in June. The estimated values of phosphorus release into the lake quantitatively suggest that the effect of sediment over the trophic level of the lake was minimal. During the research period, total phosphorus (TP) concentrations of the sediment samples varied between 286.00 μg g~(-1) DW and 892.25 μg g~(-1) DW, and the trophic level of the lake was found to be eu-trophic. The greater proportion of phosphorus fractions preventing phosphorus release into the lake was estimated to be organically-bound (Org≈P; 36%), and this fraction was followed by the calcium-bound (Ca≈P; 35%), iron+alumi-nium-bound (Fe+Al≈P; 16%) and carbonate-bound (CO_3≈P; 13%) phosphorus fractions, respectively. With regard to low-sediment phosphorus release into the lake, the iron+ aluminium-bound fraction (Fe+Al≈P) was effective because of the high iron content of the sediment (13450-44450 μg g~(-1) DW). During the research, another effectual component in the low-release of phosphorus was a high TFe/TP ratio (mean 45.33). High sediment clay content and macro-phyte presence at the station were the other effective factors of low-sediment phosphorus release.
机译:这项研究是在2004年7月至2005年6月之间进行的,目的是确定莫干湖沿岸沉积物中磷的季节和空间格局,以及磷向湖水中的潜在释放量。沉积物和上层水样中的总磷和磷组分主要来自湖泊中选定的站点,此外,还测量了一些化学和物理参数。磷的释放量是根据与沉积物孔隙以及沉积物的含水量有关的上层水相关的可过滤正磷酸盐的总浓度估算的,扩散系数取决于温度。在研究期间,沉积物磷释放量在0.002-0.062μg.m〜(-2)d〜(-1)之间波动,11月达到最低,6月达到最高。磷向湖泊中释放的估算值定量表明,沉积物对湖泊营养级的影响最小。在研究期间,沉积物样品的总磷(TP)浓度在286.00μgg〜(-1)DW和892.25μgg〜(-1)DW之间变化,并且湖泊的营养水平正常。有营养的。阻止磷释放到湖泊中的磷组分的比例较大,据估计是有机结合的(Org≈P; 36%),然后是钙结合的(Ca≈P; 35%),铁+铝磷结合部分(Fe +Al≈P; 16%)和碳酸盐结合部分(CO_3≈P; 13%)。对于沉积物向湖中的低沉积磷释放,由于沉积物中铁含量较高(13450-44450μgg〜(-1)DW),所以铁+铝结合部分(Fe +Al≈P)是有效的。在研究过程中,低磷释放的另一个有效成分是较高的TFe / TP比(平均值45.33)。站内较高的沉积物粘土含量和大型植物的存在是降低沉积物磷释放的其他有效因素。

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