沈阳市地铁疏干水的利用探析

针对沈阳市地铁疏干水利用的现状,综合考虑沈阳市的实际情况,总结出地铁疏干水利用的几种方法,主要包括作为运河、湖泊的补换水源,用于修复、重建湿地,农业灌溉用水以及作为水源热泵的水源等。提出沈阳市地铁疏干水利用的指导思想和法律保障。     

Drainage Investment and Wetlands Loss: an Analysis of the National Resources Inventory Data

The United States Soil Conservation Service (SCS) conducts a survey for the purpose of establishing an agricultural land use database. This survey is called the National Resources Inventory (NRI) database. The complex NRI land classification system, in conjunction with the quantitative information gathered by the survey, has numerous applications. The current paper uses the wetland area data gathered by the NRI in 1982 and 1987 to examine empirically the factors that generate wetland loss in the United States. The cross-section regression models listed here use the quantity of wetlands, the stock of drainage capital, the realty value of farmland and drainage costs to explain most of the cross-state variation in wetland loss rates. Wetlands preservation efforts by federal agencies assume that pecuniary economic factors play a decisive role in wetland drainage. The empirical models tested in the present paper validate this assumption.     

Coastal landscape preference evaluation: A comparison among tourists in Greece

An evaluation of coastal landscape of pine forest in Greece by summer visitors of various nationalities was carried out. The visual preferences for a set of landscape, represented in photographs, expressed by these various nationality groups were compared. The subjects used in this research came from Greece, Germany, Italy, France, Great Britain, Austria, Yugoslavia, and Scandinavian countries. The findings show that there is an agreement over the basic preference, but, nevertheless, there are differences of opinion between the nationality groups that might be attributed to cultural influences and the effect of being familiar with their own environments. Since coastal landscape plays an important role in the tourist industry, these findings could be very useful to policy-making agencies.     

Soft intervention technology as a tool for integrated coastal zone management

After introducing soft defence techniques as an alternative to hard defence techniques, the need is emphasized to consider the coastal area as an integral system. By recalling the main driving factors for coastal management: conflict resolution, resilience and sustainability, we logically arrive at the concepts of ecological engineering and ecotechnology, which are increasingly acknowledged as possible solutions to achieve sustainable use of coastal space as a resource. In this context, we refer to the principles of self design and of ecosystem conservation. In order to deal with real situations we are in need of fundamental ‘tools’ for the application of the soft intervention technology approach. We therefore introduce the concept of physiographic units and develop an initial elaboration for a coastal stretch and for coastal wetlands. The latter deserve more attention because of the already established practices of ecotechnology, at least as far as water and soil quality are concerned, but certainly also concerning morphology, especially in the future. We conclude by briefly discussing how activities undertaken in two research projects currently being conducted under the framework of the Marine Science and Technology Program of the Commission of the European Communities are expected to contribute to the concepts introduced here.     

子牙新河下游湿地土壤重金属垂直分布及形态特征

2014年秋季在子牙新河下游湿地采集柱状土壤样品,分析了Cd、Zn、Cu、Pb的垂向分布特征,利用Tessier连续浸提法,分析了典型湿地N1、N3、B3的重金属形态.研究结果表明,Cd、Zn、Cu、Pb含量垂向分布差异性比较大,波动幅度比较大,多数点位Cd、Cu、Zn在11-19 cm深度处出现峰值,可能与过去金属的输入和周期性淹水有关.Zn、Cu、Pb形态分布为残渣态 > 铁锰氧化物结合态 > 有机物结合态 > 可交换态 > 碳酸盐结合态,Cd形态分布为铁锰氧化物结合态 > 可交换态 > 残渣态 > 有机物结合态 > 碳酸盐结合态,Cd的生物有效性较高.湿地淹水条件影响到湿地重金属Cd的交换态和铁锰氧化物结合态的垂直分布.Cd主要以铁锰氧化物结合态的形式存在于湿地土壤中,其百分含量占53.2%,而重金属Zn、Cu、Pb主要以残渣态的形式存在于湿地土壤中,其百分含量均高于60%.根据风险评价编码法（RAC）对重金属的化学形态进行风险评价,风险顺序为：Cd>Zn>Cu>Pb,因此重金属Cd应引起足够的重视.     

Long-Term Relationship between Phosphorus Inputs and Wetland Phosphorus Concentrations in a Northern Everglades Marsh

Assessments of long-term relationships between changes innutrient inputs and wetland nutrient concentrations can becomplicated by fluctuations in other environmental factors aswell as by problems typical of long-term monitoring data.Consequently, statistical analysisof these types of data sets requirescareful consideration of environmental covariates, potentialbiases in the monitoring design, and irregularities caused bychanges in field sampling protocols. We evaluated therelationship between anthropogenic phosphorus (P) inputs andwater-column total P (TP) concentrations in a northernEverglades marsh by statistically analyzing available datacollected from several sampling programs over the past 20 years(1978–1997). Canal inputs of agricultural runoff contributemost of the P to the marsh and have produced a zone ofenrichment within the marsh during the past few decades.Regression analyses showed that both canal and marsh TPconcentrations increased during the 1980s and then decreased inthe 1990s. However, the statistical relationship between canal Pinputs and marsh TP, while significant, generally was weakexcept for marsh locations adjacent to the canal. Strongerrelationships existed between marsh TP and hydrologic parameterssuch as marsh water depth, which is controlled by changes inweather patterns and marsh management. In particular, dryconditions during the 1980s may have contributed to observedincreases in marsh P concentrations and the movement of a P`front' further into the marsh. Higher rainfall and water depthsand agricultural best management programs initiated during the1990s have been associated with reduced P concentrations incanal waters entering the marsh. While it is anticipated thatthis reduction eventually will result in lower marsh TPconcentrations, this effect is not yet evident, possibly due tointernal loading of P from enriched marsh soils. Our findingsillustrate some of the environmental factors that can complicateattempts to develop empirical relationships between P inputs andwetland P concentrations and to use such relationships to forecast changesin marsh concentrations based on past monitoring data alone.     

不同基质垂直流人工湿地对猪场污水季节性处理效果的研究

研究了3套不同基质垂直流人工湿地小试装置在不同季节处理猪场污水的运行效果.结果表明,垂直流人工湿地对有机污染物的去除效果随季节变化差异不明显,对有机物降解情况可用一级降解模型模拟;传统型湿地系统NH4+-N去除率在各季节稳定在52%,而沸石和沸石-煤渣型系统冬季NH4+-N去除效率分别从秋季的89.8%和93.4%下降至冬季的64.2%和73.5%,春、夏季回升至80%左右.冬季湿地系统中生物硝化与反硝化作用的减弱影响了垂直流人工湿地系统TN的去除;3套不同基质系统中,沸石-煤渣型系统各高度层硝化强度均为最高,沸石型和沸石-煤渣型系统的反硝化强度明显高于传统型系统,与实际运行过程TN去除率变化相吻合.采用沸石作为基质有利于系统的反硝化进程和TN的去除.垂直流系统对TP去除率随季节性变化波动不显著,但随着垂直流人工湿地系统的运行,基质层对TP的吸附逐渐饱和,去除效率明显下降.     

绿狐尾藻分解及其氮磷释放特征

湿地植物分解释放的有机物、氮和磷等会影响人工湿地对水体污染物的去除效率和出水水质.本研究采用尼龙分解袋法研究绿狐尾藻在水中的分解过程及氮磷释放特征.连续60 d的室内分解实验结果表明,前期(0～4 d)绿狐尾藻干物质质量损失速率快,占初始质量的30%,中后期(4～60 d)损失速率减慢,占31%.拟合的一级动力学分解速率常数为0. 014 2d-1,降解50%的干物质需48. 8 d.水体p H值变化情况:0～4 d从7. 60迅速下降到5. 63;中期趋于稳定;后期p H值回升到7. 03,与空白对照值接近.绿狐尾藻分解实验系统中溶解氧浓度从6. 30 mg·L~(-1)在1 d内快速下降到0. 61 mg·L~(-1),表明该系统一直处于厌氧状态.水中总氮浓度0～2 h迅速增加达到12. 7 mg·L~(-1),2 h～32 d逐渐降低到5. 80 mg·L~(-1),后期略有增加;总磷浓度初期快速升高到18. 4 mg·L~(-1),中后期趋于稳定.有机氮(占总氮65. 7%～94. 7%)和无机磷(占总磷61%～89%)是主要的氮磷存在形态.绿狐尾藻体内总氮含量随分解时间逐渐增加,从24. 3 mg·g~(-1)上升到60. 5 mg·g~(-1);而总磷含量从6. 09 mg·g~(-1)下降到2. 94 mg·g~(-1)后波动稳定,这可能与附着微生物对氮的吸收和固定等因素有关.本研究证实绿狐尾藻分解过程释放的氮磷营养元素会引起水体二次污染,为此采用合理的植物收割管理措施非常必要.     

潜流人工湿地系统停留时间分布与N、P浓度空间变化

通过人工湿地小试装置,研究了风车草和香蒲水平潜流人工湿地处理富营养化养殖水体过程中水力停留时间分布（RTD）特征和系统内N、P浓度空间变化规律.结果表明,供试的香蒲潜流湿地和风车草潜流湿地系统RTD曲线特征值σ²分别为0.324 6和0.410 8,表明水流流态介于推流与混合流之间,风车草潜流湿地系统RTD曲线较香蒲潜流湿地平滑,水流混合流动程度较弱. 2种植物类型湿地床体总氮（TN）和氨氮（NH⁺₄-N）浓度在垂直方向上的分层现象明显,尤其在湿地床体前端;TN浓度随着取样点深度增加而上升,而NH⁺₄-N浓度则以中层取样点为最低;对于总磷（TP）和正磷酸盐（PO^3-₄-P）浓度, 2种植物类型湿地系统内均表现为随取样点深度增加而上升,但这种差异随沿程而降低. 与香蒲湿地相比较,风车草潜流湿地系统N、P浓度分层现象更为明显.风车草湿地系统后端各层取样点TN和TP平均浓度较香蒲湿地系统分别下降了19.8%和12.3%,说明风车草潜流湿地系统对富营养化养殖水体中氮、磷的去除效果优于香蒲湿地.     

硝化作用对盐碱湿地N2O排放的影响及其环境因子分析

湿地是温室气体氧化亚氮(N_2O)重要的源或汇,盐碱湿地作为湿地的重要组成部分,研究其N_2O排放对于探究盐碱湿地N_2O产生的硝化作用机制及评估其在温室效应中的作用具有重要意义.本文对代表性盐碱湿地——扎龙芦苇沼泽湿地生长季的N_2O释放量及相关环境因子进行了研究.结果表明,生长季N_2O通量呈波动性下降趋势,最大值出现在7月中旬,平均排放通量为(37. 49±15. 75)μg·(m2·h)-1,表现为N_2O的释放\"源\". N_2O通量与不同深度土层温度存在显著正相关关系(P 0. 05),且上层土温对N_2O排放的影响程度高于深层土;淹水期间N_2O通量与积水深度呈显著负相关关系(P 0. 05);且土壤TOC和TN含量较低,N_2O通量与0～40 cm土层NH+4-N含量呈显著正相关关系(P 0. 05),而与NO-3-N含量没有关系,硝化作用程度要比反硝化强;此外,土壤氨氧化菌活性与0～20 cm土层温度存在极显著正相关关系(P 0. 01),且N_2O通量与氨氧化菌活性也呈极显著的线性正相关关系(P 0. 001),表明盐碱湿地的N_2O释放受硝化作用影响巨大.