基于盲数的水体沉积物潜在生态风险评价方法

基于生态风险评价系统中多种不确定性共存或交叉存在的特性,将盲数理论应用于水体沉积物潜在生态风险的评价研究。在将Hakanson潜在生态风险指数模型参数定义为盲参数的基础上,建立了沉积物潜在生态风险评价的盲数模型,并提出了污染程度和潜在生态风险等级识别盲数可靠性计算模型。根据上述盲数模型,不仅可以得到沉积物污染程度和潜在生态风险的可能取值区间,也可以得到各区间相应的可信度水平,进而定量计算待评价对象隶属于各评价等级的主观可能性大小。作为案例,将上述模型应用于巢湖十五里河河口沉积物中重金属潜在生态风险评价的研究。在得到沉积物中单个重金属污染物(Hg,Cd,Pb,Cu,Cr)隶属于污染程度各等级和潜在生态风险各等级可信度水平的基础上,得出十五里河河口处于较高生态风险水平的结论,相应的可信度为0.626。实例研究表明,以盲数理论评价沉积物的潜在生态风险,理论上可行,评价结论可信。     

青海湖生态系统健康评价

生态系统健康是一个新概念。对湖泊生态系统来说，目前尚没有统一的评价指标和评价方法。利用Xu等(1999)提出的指标体系对青海湖1988—1989年的生态系统健康状况进行评价。结果表明：青海湖生态系统健康在秋季最好，其次为夏季和春季，冬季最差。该结果客观地反映了青海湖的实际情况。     

七里海湿地的生态修复

七里海——地处天津市宁河县西南部，属典型的沼泽湿地，国家级古海岸与湿地自然保护区。近年来，它的面积不断缩小，水源枯竭，区域分割，植物群落衰颓，动物种类减少。针对上述问题分别提出了相应的生态修复对策与建议。     

湖水中磷形态的生物有效性

本文采用化学分析将湖水中的磷划分为七种形态：总磷（ＴＰ）、总反应磷（ＴＲＰ）。总溶解磷（ＴＳＰ）、溶解反应磷（ＳＲＰ）、溶解的水解性磷（ＳＨＰ）、溶解的光解性磷（ＵＶＳＲＰ）以及颗粒磷（ＰＰ）。为了确定生物有效磷，把湖水灭菌后再接入羊角月芽藻进行试验，研究了湖水中各种磷形态对羊角月芽藻最大生长量的影响。结果表明：当湖水中磷含量大于１００μｇ／ｌ时，藻的最大生长量与大多数磷形态有较好的相关性（ｎ＝１     

五里湖不同疏浚深度沉积物对氮磷释放的影响

对太湖东五里湖区污染沉积物样模拟了3种不同疏浚深度(0cm、30cm和60cm)下的60d形态氮磷释放实验,并对沉积物间隙水中氮磷的变化进行了分析。研究结果表明:疏浚与未疏浚比较,疏浚初期的0~10d内,沉积物对上覆水NH4 -N、NO2--N和TN释放增大,NO3--N释放减小,与疏浚后沉积物扩散层变薄和好氧环境的抑制有关,而对PO43--P、TP疏浚后次日出现短暂的释放现象外,此后均处于明显的磷释放受抑状态;疏浚约10d后,沉积物各氮磷形态释放出现分异现象,沉积物对水体的TN和TP释放受到显著抑制,其中20d后上覆水中NH4 -N含量的上升和PO43--P的缓慢增加,预示着底泥疏浚后仍有内源负荷回复的可能。     

应用多变量脸谱图进行河流与湖泊表层沉积物重金属污染状况的综合对比研究

依据沉积学原理和水体沉积物重金属的环境地球化学特征,将地积累指数与改进的多变量Chernoff脸谱图相结合,选择江西德兴铜矿附近的乐安江表层沉积物以及德国西南部Mannheim和Worms周围若干湖泊的表层沉积物作为研究对象,开展不同地域、不同类型水体沉积物中重金属积累的对比分析和污染状况的综合性定量评价.多变量脸谱图能清晰地反映出两区域沉积物中重金属的污染特征和空间分布模式.     

气相色谱-质谱联用测定土壤及底泥样品中的多环芳烃和硝基多环芳烃

采用气相色谱-质谱联用法测定了某化工厂火灾后周边土壤和底泥中的多环芳烃(PAHs)和硝基多环芳烃(Nitro-PAHs).结果表明,距离爆炸地点最近的几个采样点PAHs的含量均在16.61μg·g-1以上,其中厂东北采样点的PAHs总含量甚至高达417.4μg·g-1,污染最为严重;部分样品中检测到三环以下的硝基多环芳烃,三环以上的几乎均未检出.说明在燃烧爆炸过程中产生了多环芳烃,但没有显著产生高致癌性、致突变性的硝基多环芳烃.     

Seasonal variations of organic-carbon and nutrient transport through a tropical estuary (Tsengwen) in southwestern Taiwan

This paper reports the fluvial fluxes and estuarine transport of organic carbon and nutrients from a tropical river (Tsengwen River), southwestern Taiwan. Riverine fluxes of organic carbon and nutrients were highly variable temporally, due primarily to temporal variations in river discharge and suspended load. The sediment yield of the drainage basin during the study period (1995–1996, 616 tonne km^–2 year^–1) was ca. 15 times lower than that of the long-term (1960–1998) average (9379 tonne km² year^–1), resulting mainly from the damming effect and historically low record of river water discharge (5.02 m³ s^–1) in 1995. The flushing time of river water in the estuary varied from 5 months in the dry season to >4.5 days in the wet season and about 1 day in the flood period. Consequently, distributions of nutrients, dissolved organic carbon (DOC) and particulate organic carbon (POC) were of highly seasonal variability in the estuary. Nutrients and POC behaved nonconservatively but DOC behaved conservatively in the estuary. DOC fluxes were generally greater than POC fluxes with the exception that POC fluxes considerably exceeded DOC fluxes during the flood period. Degradation of DOC and POC within the span of flushing time was insignificant and may contribute little amount of CO₂ to the estuary during the wet season and flood period. Net estuarine fluxes of nutrients were determined by riverine fluxes and estuarine removals (or additions) of nutrients. The magnitude of estuarine removal or addition for a nutrient was also seasonally variable, and these processes must be considered for net flux estimates from the river to the sea. As a result, nonconservative fluxes of dissolved inorganic phosphorus (DIP) from the estuary are –0.002, –0.09 and –0.59 mmol m^–2 day^–1, respectively, for dry season, wet season and flood period, indicating internal sinks of DIP during all seasons. Due to high turbidity and short flushing time of estuarine water, DIP in the flood period may be derived largely from geochemical processes rather than biological removal, and this DIP should not be included in an annual estimate of carbon budget. The internal sink of phosphorus corresponds to a net organic carbon production (photosynthesis–respiration, p–r) during dry (0.21 mmol m^–2 day^–1) and wet (9.5 mmol m^–2 day^–1) seasons. The magnitude of net production (p–r) is 1.5 mol m^–2 year^–1, indicating that the estuary is autotrophic in 1995. However, there is a net nitrogen loss (nitrogen fixation–denitrification < 0) in 1995, but the magnitude is small (–0.17 mol m^–2 year^–1).     

蟹类活动对河口潮滩沉积物重金属分布的影响

利用现场样方调查以及室内蟹箱模拟试验,研究了蟹类的掘穴、取食等活动对河口潮滩沉积物中Cu、Pb、Fe、Mn、Zn、Cr等重金属分布的影响.结果表明,蟹类活动可以显著地增加潮滩沉积物用以交换的表面积,改变周围沉积物的有机质含量和粒度特征,使沉积物中的重金属含量显著增加,为在沉积物-水界面发生的重金属交换过程提供了更多的物质来源.蟹类活动对沉积物中重金属垂向分布的影响与沉积物类型密切相关.图6表1参10     

稻田施用沼渣对甲烷排放通量的影响

通过网室小区试验，观测得出：（１）４种沼渣处理和单施化肥处理的一季稻田平均甲烷排放通量为０．５６９～２．１８８ｍｇ０￣２·ｈ，两者无显著差异；农家肥处理稻田的平均甲烷排放通量为４４．１８ｍｇ／ｍ￣２·ｈ显著高于前两种处理，表明施用沼渣和化肥比施用农家肥能显著减少稻田甲烷排放量；（２）各处理稻田甲烷排放通量峰值期部出现在水稻蘖期至拔节初期，表明这一时期是控制稻田甲烷排放总量的关键时间；（３）各处理甲烷排放通量分别与淹水前各处理土壤及供试有机肥的易矿化碳含量、ＣＨ＿４－Ｃ含量呈显著正相关关系，这表明土壤易矿化碳含量是形成稻田甲烷的重要条件；（４）各处理之间水稻产量没有明显差异。