湖泊底泥挖掘可能导致水体氮磷平衡破坏的研究

挖掘底泥是减少富营养化湖泊内源性氮、磷元素的主要手段 ,但若挖掘不当 ,则一段时间内可能会导致水体氮、磷平衡破坏 ,富营养化加剧。从底泥挖掘可能导致水体营养元素平衡破坏的成因入手 ,探讨避免水体富营养化加剧的对策。  

气相色谱-脉冲火焰光度检测器测定痕量有机磷农药

在水样和土壤样中分别加入二氯甲烷和丙酮，用超声波提取水样中敌敌畏、乐果、甲基对硫磷、马拉硫磷、对硫磷等5种有机磷农药和土壤样中甲拌磷、二嗪磷、异稻瘟净、杀螟农、溴硫磷、水胺硫磷、稻丰散、杀扑磷等8种有机磷农药，大大地简化了测定的预处理过程。应用气相色谱法HP—5石英毛细管柱分离，脉冲式火焰光度检测器检测，取得了较好的测定结果。水样中农药的检测限≤0．O02mg／L，土壤样中农药的检测限≤0．O02mg／kg，相对标准偏差水样＜7％，土壤样＜10％，加标回收率水样在84％—96％之间，土壤样在80％—108％之间，均满足测定要求。  

五里湖—梅梁湖磷污染调查

通过对五里湖-梅梁湖洗涤剂“禁（限）磷”前后水体磷含量变化的调查，表明，禁止使用含磷洗衣粉两年后，五里湖水体中总磷含量降低20%，梅梁湖总磷含量也有下降趋势，但是五里湖近5年的总磷监测结果均超过《地表水环境质量标准》（GHZB1-1999）中Ⅴ类标准。指出，洗衣粉中所含的磷是湖区磷污染的重要来源，而水体磷负荷的大量来源是人体排泄、农业面源（含畜禽、水产养殖）和工业点源。提出，“治前”（禁磷）是前提，“治后”（除磷）是手段，根本的一条是控制入湖的总磷量，维持湖体生态平衡。  

Sequential fractionation of phosphorus in lake sediments of Northern Greece

The amounts and forms of potentially mobile P in surface sediments from two lakes, Volvi and Koronia, located in Northern Greece were evaluated using a sequential chemical extraction. Five sedimentary P reservoirs were separately quantified: loosely sorbed P (NH₄Cl-P); iron associated P (BD-P); calcium bound P (HCl-P); metal oxide bound P (NaOH-P) and residual P (organic and refractory P). Samples were taken in two seasons and the average concentration of the fractions of phosphorus were calculated. The results indicated that the TP content and chemically extractable phosphorus in the sediments of Koronia Lake were higher than those of Volvi Lake. Sediment TP was also strongly and positively correlated with sediment Fe. Fine-sized sediments exhibited significantly higher concentrations for both lakes than the sand fraction. The P in the surface sediment mainly consisted of HCl-P and Res-P, while NH₄Cl-P and BD-P only constituted a minor part. The rank order of the different P extracts was the same for the two lakes and was Residual-P > HCl-P > NaOH-P > BD-P > NH₄Cl-P.  

淮河支流污染物综合降解系数动态测算

确定河流污染物综合降解系数动态变化规律对提高水环境容量测算精度和水环境管理具有重要意义。通过现场模拟法,采用一维稳态模型测算了淮河支流洪河五沟营-塔桥乡河段COD、氨氮和总磷在枯水期、平水期和丰水期的综合降解系数,COD、氨氮和总磷降解系数在各水期的关系为枯水期<平水期<丰水期,提出了建议值并利用实测浓度对计算结果进行了检验,结果表明,不同水期综合降解系数吻合情况较好。  

在同一消解液中同时测定总磷和总氮

探讨了在同一消解液中同时测定总磷、总氮的分析方法。实验结果表明，选用合适的氢氧化钠和过硫酸钾的加入量，可在同一消解液中同时测定总磷和总氮，并能克服消解液保存时间短的缺点。应用本文所拟最佳条件对标样和水样进行分析，结果准确，方法实用。  

SMT法测定沉积物标准样品有机磷形态分析方法探究

目前水体沉积物中磷的分级提取没有统一的方法,不同的提取方法分析沉积物中的磷形态结果可能会有很大差异。SMT法因操作简单、重复性好而被广泛应用于沉积物磷形态分析,但是在实际操作中连续提取过程比较复杂,尤其是有机磷(OP)提取步骤比较繁琐,中间转移过程较多,分析人员人为操作等因素都会导致实验出现较大误差,通过多次实验研究发现,在此基础上还存在另外一种改进的OP提取方法。为了验证改进法是否具有合理可行性,以水系沉积物标准样品GSD-9和GSD-12为标样,同时以野外采集的沉积物样品为实际样品,采用标准SMT法和改进法重复测定(n=30)沉积物中OP含量。结果表明:标准SMT法提取沉积物标准样品GSD-9和GSD-12测得的OP含量分别占其总磷(TP)含量的9.33%和23.03%;改进法测得的OP含量分别占其TP含量的10.44%和23.13%,两种OP提取方法测得结果有着极高的相似性。结果表明,改进的OP提取方法具有可行性,对于沉积物OP分析提取方法的合理选择具有指导意义。  

快速固相萃取法测定食品中多种有机磷农药残留

报道了一种简便、快速的石墨碳固相萃取(SPE)食品中多种有机磷农药残留及测定的方法.采用丙酮浸泡、超声提取食品中的有机磷农药,经石墨碳固相小柱净化萃取后,用气相色谱-火焰光度检测法直接测定,加标回收率在72.0%～107%之间,RSD为6.2%～12.7%,最低检出限可达0.001 mg/kg.  

太湖氮磷浓度与水质因子的关系

在2003年10月27、28日和2004年8月19日的太湖水质试验数据基础上,研究与探讨了氮浓度、磷浓度与叶绿素a浓度、悬浮物浓度和CDOM(Colored Dissolved Organic Matter)浓度之间的定量关系。研究结果表明:①在2003年10月份和2004年8月份,太湖梅梁湾地区水体的氮、磷浓度介于1~4mg/L和0.1~0.3mg/L,该浓度恰好处于易发生水华的营养物质浓度供应区间;②与2004年8月19日相比,2003年10月27、28日的太湖藻类处于低增长、高消亡状态;③在太湖梅梁湾地区,氮、磷浓度与CDOM浓度、叶绿素a浓度和悬浮物浓度之间存在较强的线性相关性,其相关系数大于0.557;④在太湖水体中,磷浓度、CDOM浓度、叶绿素a浓度和悬浮物浓度的四因子关系模型比氮浓度、CDOM浓度、叶绿素a浓度和悬浮物浓度的四因子关系模型的相关系数高。  

A Comparison of Sediment and Monitoring Data: Implications for Paleomonitoring a Small Lake

Long-term limnological monitoring data (from 1971 to 2001) were compared with sediment core record in Lake Viitna Linajärv (hereafter L. Viitna), a small lake in northern Estonia. The monitoring data show that L. Viitna changed from mesotrophic in the 1970s to eutrophic in the 1990s. The trends of paleodata thatintegrate the changes in the biogeochemical matter cycling in the lake over 2–3 years have clear signals about changes in the state ofthe ecosystem in L. Viitna during the last decades. A gradual increase in organic productivity should reflect a greater oxygen demand in the hypolimnion. As a result the hypolimnion becameseasonally anoxic earlier and its pH level remained low for a longer time. These fundamental changes near the sediment-water interface were recorded in the sediment core. The greatest changes occurred at the beginning of the 1980s (layers at a depthof ca. 20 cm), when the meso(eu?)trophic conditions in L. Viitnastarted to become increasingly more eutrophic. The variations ofpaleorecords in the upper part of the sediment core coincide temporally with changes in the water level of the lake.