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生态学杂志 ›› 2011, Vol. 30 ›› Issue (05): 1023-1030.

• 汞的生物地球化学专辑 • 上一篇    下一篇

贵州红枫湖水体叶绿素a的分布与磷循环

商立海1,李秋华1,2,邱华北1,3,仇广乐1,李广辉1,冯新斌1**   

  1. 1中国科学院地球化学研究所环境地球化学国家重点实验室, 贵阳 550002;2贵州师范大学贵州省山地环境信息系统和生态环境保护重点实验室, 贵阳 550001;3西南大学资源环境学院, 重庆 400715
  • 出版日期:2011-05-08 发布日期:2011-05-08

Chlorophyll-a distribution and phosphorus cycle in water body of Hongfeng Reservoir, Guizhou.

SHANG Li-hai1, LI Qiu-hua1,2, QIU Hua-bei1,3, QIU Guang-le1, LI Guang-hui1, FENG Xin-bin1**   

  1. 1State Key Laboratory of Environmental Geochemistry, Institute of Geochemistry, Chinese Academy of Sciences, Guiyang 550002, China|2Key Laboratory for Information System of Mountainous Area and Protection of Ecological Environment of Guizhou Province, Guizhou Normal University, Guiyang 550001, China|3College of Resources and Environment, Southwest University, Chongqing 400715, China
  • Online:2011-05-08 Published:2011-05-08

摘要: 于2009年8月(夏季)和2010年1月(冬季)在贵州红枫湖采集了分层湖水和分层沉积物样品,分析了湖水样品的总N(TN)、总P(TP)及叶绿素a(Chl-a)含量,结果表明,湖水TN含量在2个季节无明显变化,平均含量为1.58±0.73 mg·L-1,湖水TP含量夏季(0.091±0.070 mg·L-1)高于冬季(0.026±0.055 mg·L-1)。夏季湖水在8 m处有季节性分层,下层湖水TN、TP含量高于上层;夏季湖水Chl-a主要集中在上层,上层平均含量为33.2±13.0 mg·m-3,冬季湖水Chl-a平均含量为11.1±3.7 mg·m-3,分析发现,湖水上层(8 m)Chl-a与TP有明显的线性相关关系(r=0.965,P<0.01),表明红枫湖富营养化主要受P元素限制。沉积物孔隙水中的溶解态P(DP)浓度和湖水的磷酸盐(PO3-4-P)浓度比上覆水体高,具有向上扩散的趋势,利用费克第一定律计算了沉积物向上覆水体的释P速率,发现夏季沉积物向上覆水体释P速率高于冬季,可能主要是由于夏季湖水底层的还原环境下沉积物表层的早期成岩作用生成磷酸盐进入孔隙水而促进了沉积物向上覆水体释放P。根据通量释放结果估算了全湖沉积物向水体的释P通量,约为每年5.0±5.6 t。红枫湖富营养化受P控制,沉积物向水体有很大的释放P的潜力,是湖水P的重要内源,严格控制流域的外源输入才能彻底治理该湖的富营养化。

关键词: 蚯蚓养殖, 蚓粪, 土传病害, 抑制

Abstract: In August (summer) 2009 and January (winter) 2010, water and sediment samples were collected from Hongfeng Reservoir in Guizhou to analyze the total nitrogen (TN), total phosphorus (TP), phosphate (PO3-4), and chlorophyll-a (Chl-a) in water body and the dissolved phosphorus (DP) in sediment pore water. The mean TN concentration in water body was 1.58±0.73 mg·L-1, and no obvious difference was observed between summer and winter. The mean TP concentration in water body was higher in summer (0.091±0.070 mg·L-1) than in winter (0.026±0.055 mg·L-1). In summer, the lake water at the depth 8 m was thermally stratified, with the TN and TP concentrations being higher in hypolimnion than in thermocline. The Chl-a in water body was mainly concentrated in thermocline, with a mean concentration 33.2±13.0 mg·m-3 in summer and 11.1±3.7 mg·m-3 in winter. There was a significant positive linear correlation between Chl-a and TP in the upper 8 m water layer (r=0.965,P<0.01), suggesting that the eutrophication of Hongfeng Reservoir was limited by phosphorus. The DP concentration in sediment pore water and the phosphate (PO3-4-P) concentration in water body were much higher than the PO3-4-P concentration in overlying water, which meant that the DP had a strong upward diffusion tendency. According to Fick’s first law, the phosphorus emission flux from sediment to overlying water was calculated. The phosphorus emission rate was higher in summer than in winter, possibly because the bottom anoxic water environment and its higher temperature in summer favored the formation of DP during the early diagenesis. Based on the phosphorus flux from sediment to overlying water, the annual phosphorous emission from sediment to water body was estimated as 5.0±5.6 metric tons. It was suggested that the eutrophication of Hongfeng Reservoir was controlled by phosphorous, and the sediment had a great potential in releasing phosphorous, being an important inner source of lake water phosphorous. To control the eutrophication of Hongfeng Reservoir, more strict policy was necessary to limit the anthropogenic phosphorous input from the watershed.

Key words: Vermiculture, Vermicompost, Soil borne disease, Inhibition