物理和摇蚊幼虫组合扰动对内源磷再生和形态转化的协同作用

为探讨物理和摇蚊幼虫组合扰动对内源磷再生和形态转化的协同作用,选取了苏州某富营养化河道为研究对象.利用室内静态培养试验和Rhizon间隙水采样技术,着重对比了单纯的摇蚊幼虫扰动和组合扰动下,上覆水、间隙水、沉积物中磷形态数量分布的变化规律.结果表明,组合扰动下,上覆水中不同形态磷含量(TP、PP、DTP、DIP)均处于较高水平,明显高于摇蚊幼虫扰动.这可归因于微生物活性的显著增加.与摇蚊幼虫扰动相比,组合扰动下,间隙水中DIP和Fe2+浓度的降低幅度和降低范围明显更大.这主要是由于物理扰动和底栖生物扰动产生的叠加效应,导致溶解氧渗透深度增加.另外,0~2 cm沉积物中,NH4Cl-P含量明显降低,Fe/Al-P明显增加,并且,NH4Cl-P和Fe/Al-P的变化幅度均在组合扰动下最大.这暗示了物理扰动和底栖生物扰动对磷再生和迁移产生的叠加效应.     

桑沟湾表层沉积物性质及对磷的吸附特征

通过研究桑沟湾表层沉积物对磷的吸附动力学曲线和吸附等温线,并结合沉积物的表面电荷性质及磷的形态分析,考察了沉积物对磷的吸附性能和吸附机制.结果表明,桑沟湾表层沉积物对磷的吸附过程包括快吸附过程和慢吸附过程,可用快慢二段一级动力学方程描述,等温线符合Langmuir交叉式模型.夏季沉积物样品的最大吸附量高于春季样品,粒级较小的沉积物吸附能力较强.沉积物样品对磷的最大吸附量Qm在0.047 1~0.123 0 mg·g-1之间,吸附/解吸平衡磷浓度(EPC0)范围在0.059 6~0.192 7 mg·L-1,沉积物充当"磷源"的作用.不同站位表层沉积物中无机磷(IP)是磷在沉积物中的主要赋存形态,吸附后的沉积物样品中弱吸附态磷(Ex-P)、铁结合态磷(Fe-P)明显增加.吸附过程包括物理吸附和化学吸附,以物理吸附为主.     

苦土和氧化镁处理氮磷废水的对比研究

分别采用苦土、纯氧化镁为沉淀剂对模拟高浓度氮磷废水(N/P=0.8)进行了脱氮除磷研究,比较了沉淀剂投加量、pH对2种沉淀剂处理氮磷废水的影响,对沉淀产物进行XRD分析,并进行了经济效益比较。结果表明,pH是影响2种沉淀剂处理氮磷废水的主要因素,随着pH的增加,脱氮除磷效果提高,在平衡pH为9～10之间时氮磷处理效果最佳,pH继续增加,由于磷酸镁沉淀的形成使得氨氮去除率降低。此外,处理相同的废水,苦土的最佳投加量要大于纯氧化镁,但是经济效益比较结果表明,以苦土为沉淀剂处理氮磷废水可大大降低处理成本。     

微波消解-流动注射分光光度法测定土壤中的总磷

采用热效率高的微波消解系统对土壤中的总磷进行消解,建立了微波消解-流动注射分光光度法测定土壤中总磷的方法,该方法对比HJ632-2011碱熔-钼锑抗分光光度法具有快速、简便、节约试剂等特点。本文用两种分析方法对实际土壤样品及标准样品进行定量测定,所得结果表明微波消解法能快速测定大量土壤样品的总磷。     

鸟粪石结晶法从废水中回收磷的研究进展

鸟粪石结晶法是一种能同时回收废水中磷源和氮源的处理方法。本文总结了鸟粪石晶体的生长机理、颗粒形成和生长的影响因素,并着重比较了能够形成鸟粪石的各种反应器的优缺点。此外,文章总结了采用鸟粪石结晶法处理实际废水的相关研究,并对其经济效益做了评估。最后对鸟粪石结晶技术未来的研究方向进行了展望,提出了国内鸟粪石结晶技术研究的必要性。     

碳酸根对磷酸钙沉淀反应回收磷的影响简

以模拟的厌氧消化液为处理对象，通过小试实验，考察不同初始磷浓度C_P、Ca/P物质的量比、pH和温度下，碳酸根（CO₃^2-）对磷酸钙沉淀反应回收磷的影响；利用扫描电镜（SEM）、X射线衍射仪（XRD）和傅里叶变换红外光谱（FTIR）对沉淀产物进行表征。结果表明，高浓度的CO₃^2-对以磷酸钙沉淀反应去除和回收磷的效率影响较大；C_P相同时，CO₃^2-浓度（C_CO3^2-）越大，P的去除率越低，低C_P（20 mg/L）时尤为显著；当C_CO3^2-相同时，随着C_P的增大，反应速率加快，P的去除率逐渐升高，但升高幅度越来越小；增大Ca/P比和pH能提高P的去除率，降低CO₃^2-对磷酸钙沉淀反应的抑制作用，综合考虑实际效果，应选择Ca/P比为3.33，pH为9.0作为适宜的反应条件；升高温度对降低CO₃^2-对磷酸钙沉淀反应的抑制作用贡献不大。在C_P为60 mg/L，Ca/P比为1.67，pH为9.0，温度为20℃的条件下，当C _CO3^2-为0时，得到的沉淀产物主要为羟基磷灰石HAP；当C _CO3^2-为30 mmol/L时，得到的沉淀产物为磷酸钙和碳酸合磷灰石的混合物。     

不同因素对人工湿地基质脱氮除磷效果的影响

在人工配制的污水中投入一定量的基质,不同条件下振荡培养,评价沸石、炉渣和陶瓷滤料3种基质在不同因素影响下对氨氮(NH4+-N)和总磷(TP)的吸附能力。结果表明,不同吸附时间时,沸石对NH4+-N的吸附效果最好,陶瓷滤料对TP的吸附效果最好;进水浓度对沸石吸附NH4+-N的影响较大,其吸附量随进水浓度的增大而增大,进水浓度对炉渣和陶瓷滤料吸附NH4+-N及炉渣吸附TP影响不大;3种基质对NH4+-N和TP的吸附量均是随吸附剂量的增加而降低,要达到较好的去污效果,应根据实验结果考虑基质投入量;pH值对沸石吸附NH4+-N影响显著,pH值6～7范围内吸附效果最好,pH值8～12的碱性条件有利于基质对TP的吸附。     

Observations of Atmospheric Nitrogen and Phosphorus Deposition During the Period of Algal Bloom Formation in Northern Lake Taihu,China

Cyanobacterial blooms in Lake Taihu occurred at the end of April 2007 and had crucial impacts on the livelihood of millions of people living there. Excessive nutrients may promote bloom formation. Atmospheric nitrogen (N) and phosphorus (P) deposition appears to play an important role in algal bloom formation. Bulk deposition and rain water samples were collected respectively from May 1 to November 30, 2007, the period of optimal algal growth, to measure the bulk atmospheric deposition rate, wet deposition rate, and dry deposition rate for total nitrogen (TN; i.e., all species of nitrogen), and total phosphorus (TP; i.e., all species of phosphorus), in northern Lake Taihu, China. The trends of the bulk atmospheric deposition rate for TN and the wet deposition rate for TN showed double peaks during the observation period and distinct influence with plum rains and typhoons. Meanwhile, monthly bulk atmospheric deposition rates for TP showed little influence of annual precipitation. However, excessive rain may lead to high atmospheric N and P deposition rates. In bulk deposition samples, the average percentage of total dissolved nitrogen accounting for TN was 91.2% and changed little with time. However, the average percentage of total dissolved phosphorus accounting for TP was 65.6% and changed substantially with time. Annual bulk atmospheric deposition rates of TN and TP during 2007 in Lake Taihu were estimated to be 2,976 and 84 kg km⁻² a⁻¹, respectively. The results showed decreases of 34.4% and 78.7%, respectively, compared to 2002–2003. Annual bulk deposition load of TN for Lake Taihu was estimated at 6,958 t a⁻¹ in 2007 including 4,642 t a⁻¹ of wet deposition, lower than the values obtained in 2002–2003. This may be due to measures taken to save energy and emission control regulations in the Yangtze River Delta. Nevertheless, high atmospheric N and P deposition loads helped support cyanobacterial blooms in northern Lake Taihu during summer and autumn, the period of favorable algal growth.     

Development of a Quantitative Pasture Phosphorus Management Tool Using the SWAT Model1

Abstract: Assessment tools to evaluate phosphorus loss from agricultural lands allow conservation planners to evaluate the impact of management decisions on water quality. Available tools to predict phosphorus loss from agricultural fields are either: (1) qualitative indices with limited applicability to address offsite water quality standards, or (2) models which are prohibitively complex for application by most conservation planners. The purpose of this research was to develop a simple interface for a comprehensive hydrologic/water quality model to allow its usage by farmers and conservation planners. The Pasture Phosphorus Management (PPM) Calculator was developed to predict average annual phosphorus (P) losses from pastures under a variety of field conditions and management options. PPM Calculator is a vastly simplified interface for the Soil and Water Assessment Tool (SWAT) model that requires no knowledge of SWAT by the user. PPM Calculator was validated using 33 months of data on four pasture fields in northwestern Arkansas. This tool has been extensively applied in the Lake Eucha/Spavinaw Basin in northeastern Oklahoma and northwestern Arkansas. PPM Calculator allows conservation planners to take advantage of the predictive capacity of a comprehensive hydrologic water quality model typically reserved for use by hydrologists and engineers. This research demonstrates the applicability of existing water quality models in the development of user friendly P management tools.     

高效菌藻塘系统对农村污水中磷的强化去除效果研究

研究了高效菌藻塘系统处理太湖地区农村生活污水除磷效果及其强化措施。高效菌藻塘和水生生物塘HRT分别为8 d和4 d，进水总磷浓度为1.7～17.1 mg/L，出水总磷浓度全年平均值为3.33 mg/L，高效菌藻塘系统的除磷能力欠佳。通过降低水生生物塘内水深、采用废弃石膏作为填料构建了新型复合水生生物塘，HRT=1.6 d条件下，复合水生生物塘出水总磷可保持在1 mg/L以下，可达到GB18918-2002一级B排放标准。