Dong Dan-Ping, Zhang Ting-Xi, Zhang Ding-Yu, Wang Qiao-Yun, Li De-Fang, Wang Guo-Xiang
School of Geography Science, Nanjing Normal University, Nanjing 210023, China.
Jiangsu Center for Collaborative Innovation in Geographical Information Resource Development and Application, Nanjing 210023, China.
Huan Jing Ke Xue. 2016 Nov 8;37(11):4194-4202. doi: 10.13227/j.hjkx.201603057.
Potential release of phosphorus in lake sediments depends largely on the fractions and distribution of organic phosphorus. MaoDu was chosen as the research area in the west of Lake Taihu. The chemical forms of the surface sediments were investigated by the Ivannoff extraction methods. The results showed that the main organic phosphorus form of sediments at different sampling places was humic acid-OP. It accounted for 35% of the total organic phosphorus. Horizontal distribution: Total organic phosphorus content from the shore to the middle of total showed a trend of rising after decline; vertical distribution: Total organic phosphorus content was the lowest in 2-6 cm and the highest in 4-8 cm. Various phosphorus content followed the order of humic acid-OP > residual-OP > HCl-OP > fulvic acid-OP; the relative content of NaHCO-OP in the total organic phosphorus content showed a trend of rising followed by reduction and then rising again from the shore to the middle, cyanobacteria residue deposition increased the content of NaHCO-OP in sediment. Contents of NaHCO-OP and humic acid-OP both first reduced, then increased and finally reduced in the vertical distribution, the content of NaHCO-OP was the lowest in 4-6 cm and humic acid-OP was the highest in 4-8 cm. HCl-OP and fulvic-OP decreased with increasing depth in the vertical distribution. The content of residual-OP showed stable tendency in the vertical direction and was about 45 μg·g. Labile OP and pH, DO, the depth of water were significantly negatively correlated, OM and NaOH-Pi were significantly correlated with total organic phosphorus, labile OP, moderately labile OP and nonlabile OP. Three components of organic phosphorus had bio-availability and played an important role in lake eutrophication. The increase of the content of labile OP might promote the black water aggregation (BWA) in cyanobacteria accumulation.
湖泊沉积物中磷的潜在释放很大程度上取决于有机磷的形态和分布。选取太湖西部的茅渚作为研究区域。采用伊万诺夫萃取法研究表层沉积物的化学形态。结果表明,不同采样点沉积物中主要的有机磷形态为腐殖酸磷。它占总有机磷的35%。水平分布:总有机磷含量从岸边到湖心总体呈先下降后上升的趋势;垂直分布:总有机磷含量在2 - 6厘米处最低,在4 - 8厘米处最高。各类磷含量顺序为腐殖酸磷>残渣态磷>盐酸提取态磷>富里酸磷;总有机磷中碳酸氢钠提取态磷的相对含量从岸边到湖心呈先上升后下降再上升的趋势,蓝藻残体沉积增加了沉积物中碳酸氢钠提取态磷的含量。碳酸氢钠提取态磷和腐殖酸磷在垂直分布上均为先降低、再升高、最后又降低,碳酸氢钠提取态磷在4 - 6厘米处含量最低,腐殖酸磷在4 - 8厘米处含量最高。盐酸提取态磷和富里酸磷在垂直分布上随深度增加而降低。残渣态磷在垂直方向上呈稳定趋势,约为45μg·g。活性磷与pH、溶解氧、水深显著负相关,有机质和氢氧化钠提取态无机磷与总有机磷、活性磷、中度活性磷和非活性磷显著相关。有机磷的三个组分都具有生物有效性,在湖泊富营养化中起重要作用。活性磷含量的增加可能促进蓝藻聚集区黑水团的形成。