首页> 外文期刊>Environmental toxicology and chemistry >TEMPORAL AND VERTICAL DISTRIBUTION OF TOTAL AMMONIA NITROGEN AND UN-IONIZED AMMONIA NITROGEN IN SEDIMENT PORE WATER FROM THE UPPER MISSISSIPPI RIVER
【24h】

TEMPORAL AND VERTICAL DISTRIBUTION OF TOTAL AMMONIA NITROGEN AND UN-IONIZED AMMONIA NITROGEN IN SEDIMENT PORE WATER FROM THE UPPER MISSISSIPPI RIVER

机译:密西西比河上游沉积物孔隙水中总氨氮和非离子化氨氮的时间和垂直分布

获取原文
获取原文并翻译 | 示例
       

摘要

We examined the temporal and vertical distribution of total ammonia nitrogen (TAN) and un-ionized ammonia nitrogen (NH_3-N) in sediment pore water and compared the temporal patterns of TAN and NH_3-N concentrations in overlying surface water with those in pore water. Pore water was obtained by core extraction and subsequent centrifugation. We measured TAN concentrations and calculated NH_3-N concentrations from February through October 1993 at four sites in Pool 8, upper Mississippi River, at depths of 0 to 4, 4 to 8, and 8 to 12 cm below the sediment-water interface. Total ammonia nitrogen and NH_3-N concentrations were significantly different among sampling dates (p = 0.0001) and sediment depths (p = 0.0001). Concentrations of TAN and NH_3-N in surface water were significantly less than those in pore water from all sediment depths (p < 0.05). Concentrations in pore water ranged from 0.07 to 4.0 mg TAN/L and less than 1 to 20 μg NH_3-N/L in winter, and from 0.07 to 10.0 mg TAN/L and 1 to 175 μg NH_3-N/L in summer; greatest concentrations were usually found in sediments 8 to 12 cm deep. Annual mean TAN concentrations were positively correlated with silt and volatile solids content and were negatively correlated with sand content. Because of the high variability of TAN and NH_3-N concentrations in pore water, sediment toxicity studies should take into account the season and the depth at which sediments are obtained. The annual mean NH_3-N concentration in pore water at one site (55 μg/L) exceeded the concentration (30 μg/L) demonstrated to inhibit growth of fingernail clams in laboratory studies. However, these concentrations apparently were not lethal, as evidenced by the presence of fingernail clams at this site.
机译:我们研究了沉积物孔隙水中总氨氮(TAN)和非离子化氨氮(NH_3-N)的时间和垂直分布,并比较了地表水和孔隙水中TAN和NH_3-N浓度的时间分布。通过岩心提取和随后的离心分离获得孔隙水。我们测量了TAN浓度,并计算了1993年2月至10月从密西西比河上游8号水池中四个地点(沉积物-水界面以下0至4、4至8和8至12 cm)处的NH_3-N浓度。采样日期(p = 0.0001)和沉积物深度(p = 0.0001)之间的总氨氮和NH_3-N浓度显着不同。在所有沉积物深度下,地表水中的TAN和NH_3-N浓度均显着低于孔隙水中的浓度(p <0.05)。冬季,孔隙水中的浓度为0.07至4.0 mg TAN / L,小于1至20μgNH_3-N / L,夏季为0.07至10.0 mg TAN / L和1至175μgNH_3-N / L;通常在8至12厘米深的沉积物中发现最大浓度。年平均TAN浓度与淤泥和挥发性固体含量呈正相关,与沙子含量呈负相关。由于孔隙水中TAN和NH_3-N的浓度变化很大,因此沉积物毒性研究应考虑到沉积物的季节和深度。在一个场所的孔水中年平均NH_3-N浓度(55μg/ L)超过了实验室研究中显示的抑制指甲of生长的浓度(30μg/ L)。但是,这些浓度显然没有致死性,如该部位指甲蛤的存在所证明。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号