洱海入湖河口湿地干湿季沉积物氮、磷、有机质垂向分布特征及污染风险差异性

以云南洱海罗时江河口湿地为典型对象,利用柱状底泥分层采样器采集罗时江河口湿地表层(0~10 cm)、中层(10~30 cm)和底层(30~60 cm)沉积物样品,分析干、湿季沉积物总氮(TN)、总磷(TP)、有机质(OM)垂向分布特征,并对沉积物进行污染风险评价.结果表明:1干季罗时江河口湿地表层、中层和底层沉积物TN平均含量分别为1.734、1.453和1.255g·kg~(-1),TP平均值分别1.085、1.034和0.992 g·kg~(-1),OM平均值分别为59.051、47.730和42.133 g·kg~(-1);湿季罗时江河口湿地表层、中层和底层沉积物TN平均含量分别为1.147、0.948和0.895 g·kg~(-1),TP平均值分别0.599、0.523和0.519g·kg~(-1),OM平均值分别为53.098、46.897和43.395 g·kg~(-1);干、湿季各指标含量垂向分布随沉积深度的增加呈下降趋势,表层富集明显;三层沉积物各指标含量均为干季高于湿季,且除OM外,TN和TP均达到显著差异(P0.01).2单因子指数(PI)、有机氮指数(ON)和有机指数(OI)评价结果表明,整体上干季沉积物氮磷属于重度污染,有机质属于中度污染;湿季沉积物氮和有机质均为中度污染,磷为轻度污染;总体上沉积物氮、磷、有机质污染水平为干季高于湿季,且干、湿季各污染指数均为表层最高,中层次之,底层最低,表层污染最为严重.3干、湿季罗时江河口湿地污染来源存在差异,干季以外源为主,湿季以内源为主;干季沉积物营养盐潜在释放风险较湿季大,且以表层释放风险最大.     

基于合作博弈论的感潮河网区污染物排放总量削减分配模型研究

在给定污染物削减目标的情况下,如何确定各排污区域的分配比例一直是污染物总量分配技术的核心问题,博弈论是解决这一问题的有效尝试。采用合作博弈论方法,以感潮河网区各排污区域为研究对象,充分考虑各区域的污染治理成本、排污策略与环境质量的相互影响,建立了在给定污染物总削减比例条件下各区域环境合作的博弈模型,计算了各种可能联盟的特征函数值,利用Shapley值法进行合作收益的公平分配。结合珠江三角洲西江-石岐河河网区3个区域的环境合作案例说明削减合作的可行性,在总削减比例为15%的约束下,3区域合作削减比例是20.77%、12.82%和12.99%,与合作前相比,3个区域合作后环境成本分别减少了11.83%、2.13%和2%。     

Coastal Flood Inundation Monitoring with Satellite C‐band and L‐band Synthetic Aperture Radar Data

Satellite Synthetic Aperture Radar (SAR) was evaluated as a method to operationally monitor the occurrence and distribution of storm‐ and tidal‐related flooding of spatially extensive coastal marshes within the north‐central Gulf of Mexico. Maps representing the occurrence of marsh surface inundation were created from available Advanced Land Observation Satellite (ALOS) Phased Array type L‐Band SAR (PALSAR) (L‐band) (21 scenes with HH polarizations in Wide Beam [100 m]) data and Environmental Satellite (ENVISAT) Advanced SAR (ASAR) (C‐band) data (24 scenes with VV and HH polarizations in Wide Swath [150 m]) during 2006‐2009 covering 500 km of the Louisiana coastal zone. Mapping was primarily based on a decrease in backscatter between reference and target scenes, and as an extension of previous studies, the flood inundation mapping performance was assessed by the degree of correspondence between inundation mapping and inland water levels. Both PALSAR‐ and ASAR‐based mapping at times were based on suboptimal reference scenes; however, ASAR performance seemed more sensitive to reference‐scene quality and other types of scene variability. Related to water depth, PALSAR and ASAR mapping accuracies tended to be lower when water depths were shallow and increased as water levels decreased below or increased above the ground surface, but this pattern was more pronounced with ASAR. Overall, PALSAR‐based inundation accuracies averaged 84% (n = 160), while ASAR‐based mapping accuracies averaged 62% (n = 245).     

模拟SO_4~(2-)沉降对河口潮汐湿地甲烷排放通量的影响

2008年每月小潮日原位定期向闽江河口鳝鱼滩咸草(Cyperus malaccensis)潮汐湿地试验样地施加25,50,100kgSO42--S/(hm2·a)的硫酸钠溶液,探讨模拟SO42-酸沉降对河口潮汐湿地甲烷排放通量的影响.结果表明,SO42-酸沉降对于河口潮汐湿地甲烷排放通量基本无抑制作用.添加SO42-室内厌氧培养试验结果显示,虽然SO42-输入对湿地土壤CH4产生量具有一定的抑制作用,但相对对照组,下降幅度仅为8.5%~15.4%.室内添加甲烷产生基质的厌氧培养试验结果表明,非竞争性途径甲烷产生基质(甲醇和三甲胺)的添加可刺激并增加土壤的甲烷产生量,解释了原位施加SO42-对于河口潮汐湿地甲烷排放通量的基本无抑制作用的试验结果.     

Modeling the effects of constructed wetland on nonpoint source pollution control and reservoir water quality improvement

This article describes the integrated modeling approach for planning the size and the operation of constructed wetlands for maximizing retention of nonpoint source pollutant loads and reservoir water-quality improvement at a catchment scale.The experimental field-scale wetland systems (four sets,0.88 ha each) have been in operation since 2002,where water depth was maintained at 30–50 cm and hydraulic loading rate was at 6.3–18.8 cm/day.The wetland system was found to be adequate for treating polluted stream water with stable removal efficiency even during the winter.The integrated modeling system (modified-BASINS) was applied to the Seokmoon estuarine reservoir watershed and calibrated with monitoring data from constructed wetland,stream,and reservoir.The calibrated integrated modeling system estimated that constructing wetlands on 0.5% (about 114 ha) of the watershed area at the mouth of reservoir could reduce 11.61% and 13.49% of total external nitrogen and phosphorus loads,respectively.It also might improve the nitrogen and phosphorus concentration of the reservoir by 9.69% and 16.48%,respectively.The study suggested that about 0.1%–1.0% of the watershed area should be allocated for constructed wetland to meet specified water-quality standards for the estuarine reservoir at the polder area where land use planning is relatively less complicated.     

佛山水道引水对环境容量影响研究

采用污染负荷优化分配的线性规划方法,通过感潮河网水环境数学模型模拟得出污染贡献率。求取不同引水方案时佛山水道的环境容量,并建立引水量与环境容量的回归方程。研究结果表明,环境容量与引水量呈线性递增关系。根据回归方程可反推得出引水方案或削污方案,为引水与截污的实施提供了数据支持,并且对佛山水道综合整治的优化决策具有指导意义。     

氮输入对三江湿地小叶章不同生长阶段土壤产生CH_4能力的影响

在小叶章(Deyeuxia angustifolia)不同生长阶段,用室内鲜土培养法对土壤CH4的产生能力进行了研究.结果表明,氮输入后,植物各生长阶段的土壤CH4产生率均随时间的推移发生了明显的波动.从生长季(6月7日～8月24日)CH4产生率均值来看,不同氮输入水平对土壤CH4产生起促进作用;不同氮输入水平对植物不同生长阶段CH4产生率影响明显.第一(6月7日～7月2日)、第二(7月2日～7月20日)阶段适量的氮输入(6g.m-2)对CH4产生起促进作用,但过量氮输入(12g.m-2)会对CH4产生起抑制作用;而第三(7月20日～8月7日)、第四(8月7日～8月24日)阶段不同氮输入均对CH4产生起促进作用;氮输入后,土壤微生物量碳(MBC)、土壤微生物量氮(MBN)、土壤基础呼吸(BR)、土壤代谢熵(qCO2)、土壤诱导呼吸(SIR)、铵态氮(NH4+-N)、硝态氮(NO3--N)和植物地上生物量与土壤CH4产生的动态关系存在差异.土壤CH4产生与qCO2呈显著正相关(p0.01),与土壤MBN、TOC和地上生物量呈显著正相关(p0.05).     

基于COHERENS模型的污染物质输运数值模拟

以COHERENS模型为基础,建立了长江下游感潮河段三维水流及污染物质输运数学模型,该模型通过σ坐标变换,使整个水域垂直方向可采用相同的分层。基于模态分裂法,将三维流动分成表面重力波(外模式)和内重力波(内模式);模型求解技术上采用算子分裂法,使用了superbee限制器TVD格式,减小非物理的数值虚拟震荡。选取长江常熟段为例,模型较好的模拟了感潮河段三维流场及污染带分布特征。该成果对感潮地区污染物输运规律及水污染控制具有指导意义。     

Heavy metals of natural and reclaimed tidal riparian wetlands in south estuary, China

The concentrations of Cd, Cr, Cu, Ni, Pb, and Zn in two plant species (Scirpus tripueter Linn. and Cyperus malaccensis Lam.), water, and soils sampled from the reclaimed tidal riparian wetlands (RTRWs) and the natural riparian wetlands (NRWs) in the Pearl River estuary (PRE), were analyzed to investigate and compare their distribution and accumulation. The results show that the concentrations of the six studied heavy metals in soils exceed the eco-toxic threshold recommended by USEPA. The concentrations of Cd, Cr, and Zn in plants may lead to toxic effects compared to others.The hydraulic conditions and the degree of human disturbances can affect the heavy metal accumulation in RTRWs and NRWs. The heavy metal concentrations in water are higher whereas they are lower in soils of RTRWs Compared with that in the NRWs. The accumulation of heavy metals in the roots of plants is higher in NRWs than those in RTRWs while the opposite result is found for heavy metal accumulation in shoots. Based on the bioaccumulation and translocation factors, the plants in NRWs have the higher capacity to accumulate heavy metals, while higher abilities to transport heavy metals from roots to shoots are observed in RTRWs. Heavy metal contaminations in RTRWs are dominated by anthropogenic sources from both side uplands and river water, whereas in NRWs, the metal accumulations are simultaneously affected by anthropogenic and natural factors.     

海湾综合整治与资源环境优化研究进展

依据近年来国内外的研究成果,综述了海湾综合整治专项研究的内容、方法,阐述了基于数值模拟技术的海湾综合整治效果预测的研究方法.在深入分析的基础上,就海湾综合整治目前存在的问题和今后的研究工作进行了讨论,并就此提出了几点建议.