新疆绿洲生态环境与经济发展的协调关系分析

建立新疆绿洲生态环境质量综合评价指标体系和经济发展水平综合评价指标体系,利用熵值法分别测度2000年-2010年新疆绿洲生态环境质量综合水平和经济发展综合水平,在此基础上利用协调模型,测度两者的协调度和协调发展度,进而分析两者的协调关系。分析结果显示:新疆绿洲生态环境质量综合水平缓慢下降,经济发展综合水平不断上升;两者的协调关系从中级协调-优质协调-中级协调,协调发展度表明两者的协调处于相对低层次的协调。     

区域可持续发展评价方法与实例研究

１评价指标体系的建立依据科学性、可操作性、相关性、简明性原则，综合采用频率统计法、理论分析法和专家咨询法，并考虑所研究区域———青岛市崂山区的自然环境和社会经济发展状况，建立了区域可持续发展评价指标体系，见表１。２评价指标权重的确定通过专家咨询，采用群组层次分析法，求出各评价指标的权重，见表１。表１区域可持续发展评价指标体系与权重３　评价方法的选取３－１　无量纲化处理模型采用直线型模糊隶属函数，对评价指标值进行无量化处理。根据统计指标的性质及表现不同，主要有下列３种类型：（１）正指标类，其模糊隶…     

基于变异系数-综合指数法的乌鲁木齐城市脆弱性评价

从生态环境、经济和社会脆弱性三个方面,筛选新疆乌鲁木齐城市2006—2015年近十年的34个具体评价指标建立了城市脆弱性评价指标体系,通过对指标数据进行标准化处理后,以变异系数法确定各指标的权重,并运用综合指数法对乌鲁木齐城市脆弱性进行了综合评价。结果表明:伴随着经济的快速发展,乌鲁木齐城市综合脆弱性逐渐降低,但长时间处于中等偏高状态;虽然经济、社会和生态环境的综合脆弱性指数都呈下降趋势,但生态环境与经济和社会发展不协调,以牺牲环境为代价从而获得经济发展的粗放型经济发展模式仍然存在。据此有针对性地提出了有利于乌鲁木齐城市未来发展的经济、社会与生态环境相协调的经济增长模式。     

层次分析法在工业污水处理厂收水体制选择中的应用

该文基于适应于工业污水处理厂(工业废水量≥50%)的收水体制,利用层次分析法(AHP)建立4层14指标2方案的综合评价体系,并通过构造判断矩阵及一致性检验得到各指标的权重值。在此基础上,利用专家打分法建立指标评价标准和量化方法,并选择采用合流制和分流制收水体制的工业污水处理厂各8家,分别建立来水复杂程度、处理效果和投资费用之间的相关函数,从而为通过来水复杂程度选择收水体制提供理论依据和实践指导。     

晋冀鲁豫接壤区“经济─环境”系统协调状态研究

本文用协调度中的发展协调度方法对晋冀鲁豫接壤区区域“经济──环境”系统的协调状态及调控进行了研究。在经济快速增长（GNP＞8％）的前提下，用2个权重相等的子系统，即生态环境质量综合评价值Sp和发展经济的投资环境综合评价值Tp所组成的协调度综合评价值Zp的计算值判断了该区域的“经济──环境”系统的协调状态为基本不协调状态，即随着经济的快速增长，生态环境有所恶化。从2个子系统的单项指标分析了生态环境有所恶化的原因并用环境经济学中的环境管理规划的基本原理从可持续发展的角度讨论了环境和经济发展的调控对策。     

应用模糊评判法划分湘水环境功能

根据水域功能区划分的指标要求，选择ＣＯＤ＿（Ｍｎ）等１３个项目作为划分参数，通过确定隶属函数、建立模糊关系矩阵、计算权重建立归一化权重和综合评判等步骤，划分出湖南境内湘江干流１１个区段的功能性。使用此法划分水环境功能，可以通过模糊函数来体现实际监测值与各个污染级别间的亲疏关系，使结果量值化，减少人为的主观随意性。     

水利水电建设工程生态环境质量定量评价体系研究

依据国家有关法律和法规 ,根据水利水电建设项目工程的特点 ,提出了一个综合反映水利水电建设工程生态环境质量定量评价体系 ,它从一系列指标的客观实测值或估算值与该指标在生态环境中的主观环境质量评价等级两者间建立评价体系 ,并根据拟建水库的生态环境效应判别并运用特尔菲法确定各指标的权重。     

基于修正熵权法的油气管道土壤腐蚀分级量化评价方法研究

针对油气管道土壤腐蚀核心影响因素权重系数的求解存在单因素指标的不确定性,导致权值结果出现偏差,造成综合评估结果不准确这一问题,提出主客观结合的赋权方法,建立了可靠的油气管道土壤腐蚀核心影响因素权重分级量化评价模型。利用粗糙集和熵权法确定主权重和主权重值,并采用无量纲化同级变换和层次分析(AHP)法来修正模糊单因素条件属性的权重值,可得到合理的油气管道土壤腐蚀分级量化评价结果。通过与实际数据比较表明,结合AHP法修正特定区间下不定单因素指标的权重值,可以提高单因素指标权重值的精确度,获得可靠的油气管道土壤腐蚀综合评价结果。     

晋冀鲁豫接壤区“经济——环境”系统协调状态研究

本文用协调中的发展协调度方法对晋冀鲁豫接壤区区域“经济－环境”系统的协调状态及调控进行了研究。在经济快速增长的前提下，用２个权重相等的子系统，即生态环境质量综合评价值Ｓｐ和发展经济的投资环境综合评价值Ｔｐ所组成的协调度综合评价值Ｚｐ的计算值判断了该区域的“经济－环境”系统的协调状态为基本不协调状态，即随着经济的快速增长，生态环境有所恶化。从２个子系统的单英指标分析了生态环境有所恶化的原因并用环境经     

基于生态文明管理下云南省典型生态区生态监测与评估指标体系的构建

以云南省金沙江流域典型生态区为研究对象,基于PSR模型,初步建立了以自然灾害、人类活动和社会经济发展为压力因子,从景观和生态系统两个层次测度生态质量,以生态建设工程和生态专项治理措施两个方面表达人类响应的生态监测评价指标体系。利用主成分分析法、综合评价法进行指标权重赋值和生态质量综合评价。并进一步分析了传统光学遥感及激光雷达获取监测指标数据优劣性。     

厌氧氨氧化过程中COD及pH与基质浓度之间的关系

分析了上向流厌氧氨氧化生物滤池中氮素化合物浓度、COD和pH变化规律以及ANAMMOX活性和生物量的分布规律,利用数理统计的方法研究了厌氧氨氧化过程中COD和pH与氮素基质浓度之间的关系.结果表明,溶解氧和氮负荷的共同作用使得ANAMMOX活性和生物量的分布沿滤层深度呈"山脊"状不均匀分布;异养反硝化的存在和H+的消耗使得厌氧氨氧化过程中COD和pH分别呈降低和升高趋势;100 mg/L以下的有机物浓度对厌氧氨氧化菌的影响不大,且COD和pH与基质NH4+-N浓度之间呈良好的线性相关关系.本试验中COD-NH4+-N和pH-NH4+-N拟合直线的斜率分别为1.113 8±0.052 2和-0.111 3±0.001 2,置信度为95%,平均相关系数R2分别为0.982 3和0.985 0.     

基于电子鼻土壤与地下水污染修复现场TVOC和恶臭的评估

根据上海某土壤与地下水污染修复现场情况,应用自主研发的电子鼻系统(iSA-M1)分别对未修复及修复过程中的土壤和地下水、修复场地上空及周边空气中的VOCs和恶臭类气体进行检测.结合前期研究所得TPI和OPI公式,求得各点的值,并将其用图表示.结果表明:①修复后TVOC和恶臭的浓度总体呈下降趋势;②在土壤和地下水修复过程中,VOCs和恶臭的挥发受气象要素和作业的影响,其浓度在总体下降的过程中伴随着阶段性上升现象;③结合GIS技术,电子鼻能初步用于评估土壤和地下水修复现场造成的空间污染情况及对周围居民产生的影响.但造成影响程度的具体细化分级还需要进一步研究.     

军工材料环境适应性工程化验证和研究发展战略探讨

通过对国内外发展现状分析,讨论了环境适应性工程化验证和研究在军工材料开发、应用及其在武器装备发展中的地位和作用。提出了军工材料环境适应性工程化验证的技术内涵、试验与研究的模式和军工材料开发到武器装备应用各个阶段的任务和目标。在此基础上。探讨了发展军工关键材料环境适应性工程化验证试验与研究的总体战略和目标。结合国情。提出了军工关键材料环境适应性工程化验证与研究和关键材料体系环境适应性数据完善．军工关键材料环境适应性工程化验证自主保障能力建设．军工关键材料环境适应性工程化验证技术的提升等3方面重点发展和研究内容的构想与建议。     

中国资源型城市的高质量发展：困境与突破

资源型城市的高质量发展具有重大的战略意义。为清晰认识中国资源型城市转型存在的问题以及高质量发展的路径,邀请来自不同领域的十位专家就当前资源型城市高质量发展的主要困境与突破路径等研究前沿进行访谈,访谈结果表明：中国资源型城市转型取得了巨大成绩,但距离高质量发展的要求仍有较大距离,突出表现在经济发展仍未能摆脱资源依赖的发展路径、推动高质量发展的新要素集聚偏弱和碳减排目标下资源型城市的内、外部均面临着巨大的压力;新时期需要重新认识资源型城市的作用和地位,提升资源型城市保障国家资源能源安全的能力;在深刻把握传统资源禀赋概念内涵基础上实现对新资源体系的再认知,注意挖掘新资源,充实资源型城市研究的新知识体系;要针对不同类型的资源型城市的发展条件,分类施策,因地制宜推动资源型城市的创新发展;要继续提高经济增长的就业弹性,增强经济发展拉动就业的能力,并充分重视就业机会的创造和培育;要加快探索绿色、高效的转型发展道路,同步实现“存量”的绿色化和“增量”的绿色性;要综合考虑资源型城市开发基础和要素资源条件,从传统的“增长和扩张型”转变为“高效增长与精明收缩结合型”发展模式;要整合新数据与新技术方法科学/智...     

Sorption and cosorption of the nonionic herbicide mefenacet and heavy metals on soil and its components

Sorption and cosorption of the nonionic herbicide mefenacet and two typical metals (copper and silver) on black soil and its components (kaolinite and humic acid) were investigated. It was found that because of their different valences and properties, Cu²⁺and Ag⁺ presented different effects on the sorption of mefenacet. Due to the competition of Cu²⁺, along with the shells of dense water formed by its surface complexation, for sorption surface area with mefenacet, the addition of Cu²⁺ decreased the sorption amount of mefenacet on soil and its components, especially on humic acid. However, the addition of Ag⁺ significantly enhanced the sorption of mefenacet, which was attributed to the softness of the cation that weakened the hydrophilicity of the local region around Ag⁺-complexed functionalities, and thus mitigated the competitive sorption of water. In addition, the sorption of mefenacet on soil with or without the two metals was generally decreased with increasing pH, which was caused by the hydrolysis of carbonyl and carboxyl groups on the surface of the sorbents, π-π interaction between mefenacet and the soil organic matter, and so on. On the other hand, the presence of mefenacet seemed to have little effect on the sorption of Cu²⁺ and Ag⁺, indicating that Cu²⁺ and Ag⁺ might be sorbed strongly on the tested sorbents and the mefenacet added was too low in concentration to affect the sorption of the metals.     

Experimental investigation of the effect of sediment transport patterns on the adsorption of cadmium ions onto sediment particles

The mechanism of flow turbulence, sediment supply conditions, and sediment transport patterns that affect the adsorption of cadmium ions onto sediment particles in natural waters are experimentally simulated and studied in this study both in batch reactors and in a turbulence simulation tank. By changing the agitation conditions, the sediment transport in batch reactors can be categorized into bottom sediment-dominated sediment and suspended sediment-dominated sediment. It is found that the adsorption rate of bottom sediment is much less than that of suspended sediment, but the sediment transport pattern does not affect the final (equilibrium) concentration of dissolved cadmium. This result indicates that the parameters of an adsorption isotherm are the same regardless of the sediment transport pattern. In the turbulence simulation tank, the turbulence is generated by harmonic grid-stirred motions, and the turbulence intensity is quantified in terms of eddy diffusivity, which is equal to 9.84F(F is the harmonic vibration frequency) and is comparable to natural surface water conditions.When the turbulence intensity of flow is low and sediment particles stay as bottom sediment, the adsorption rate is significantly low, and the adsorption quantity compared with that of suspended sediment is negligible in the 6 h duration of the experiment. This result greatly favors the simplification of the numerical modeling of heavy metal pollutant transformation in natural rivers. When the turbulence intensity is high but bottom sediment persists, the rate and extent of descent of the dissolved cadmium concentration in the tank noticeably increase, and the time that is required to reach adsorption equilibrium also increases considerably due to the continuous exchange that occurs between the suspended sediment and the bottom sediment.A comparison of the results of the experiments in the batch reactor and those in the turbulence simulation tank reveals that the adsorption ability of the sediment, and in particular the adsorption rate, is greatly over-estimated in the batch reactor.     

持续水动力作用下湖泊底泥胶体态氮、磷的释放

为揭示水动力扰动及其后续沉淀效应对湖泊内源氮、磷营养盐释放的作用,通过室内试验模拟了水体在受到持续扰动后又长时间静置沉淀的整个过程. 结果表明,水动力扰动初期可引起底泥颗粒态和胶体态氮、磷向水体大量释放. 在连续扰动0.5 d时,水体总氮(TN)和总磷(TP)浓度分别达最高值2.106 mg/L和0.272 mg/L; 连续扰动1 d时,水体中胶体氮(CN)和胶体磷(CP)含量分别达最高值0.452 mg/L和0.052 mg/L; 之后虽继续扰动,因颗粒物和胶体物质的凝聚沉淀作用超过了其悬浮量,TN、TP、CN、CP的含量却转而降低.在停止扰动后的静置过程中,大颗粒悬浮物迅速沉淀,而胶体物质沉降缓慢,静置时间超过1 d后,CN和CP含量才开始因絮凝沉淀而降低.真溶解态氮(UDN) 和真溶解态磷(UDP)含量在扰动阶段升高较少而在静置1　d之后有持续大幅度升高,说明胶体的吸附作用在扰动阶段限制了水体溶解态氮磷含量的升高,且延长了其悬浮后在水柱中的停留时间,在扰动后的静置阶段,胶体又会将吸附的氮磷解吸释放到水体中,从而延缓了营养盐去除和水质的改善.     

污泥超高温好氧发酵去除氟喹诺酮类抗生素及其降解产物

对比分析了污泥传统高温好氧发酵(TC)和超高温好氧发酵(HTC)对诺氟沙星(NOR)、氧氟沙星(OFL)及其降解产物的去除性能.结果表明,超高温好氧与高温好氧发酵25d时NOR去除率分别为91.8％,92.1％,产物诺氟沙星脱乙基(NORP)残留含量分别为628,668μg/kg;OFL去除率分别为92.1％、88.1...     

MFI型沸石吸附分离水体中混合硝基氯苯的研究

采用MFI型沸石(HZSM-5与Silicalite-1沸石)为吸附剂分别吸附水体中的对硝基氯苯和邻硝基氯苯,研究了温度与沸石的结构特性对硝基氯苯吸附的影响,以及2种硝基氯苯分子在MFI型沸石中的扩散行为．结果表明,在不同温度下,对硝基氯苯与邻硝基氯苯在HZSM-5与Silicalite-1沸石中的吸附行为明显不同;对硝基氯苯在2种MFI型沸石中的扩散系数都显高于邻硝基氯苯．对硝基氯苯与邻硝基氯苯在吸附量与扩散性上的差异导致HZSM-5与Silicalite-1沸石对对硝基氯苯的吸附具有良好的选择性．尤其HZSM-5沸石在低温下更有利于从水体中选择性吸附分离混合硝基氯苯。     

Nitrogen cycling of atmosphere-plant-soil system in the typical Calamagrostis angustifolia wetland in the Sanjiang Plain, Northeast China

The nitrogen (N) distribution and cycling of atmosphere-plant-soil system in the typical meadow Calamagrostis angustifolia wetland (TMCW) and marsh meadow Calamagrostis angustifolia wetland (MMCW) in the Sanjiang plain were studied by a compartment model. The results showed that the N wet deposition amount was 0.757 gN/(m2·a), and total inorganic N (TIN) was the main body (0.640 gN/(m2·a)). The ammonia volatilization amounts of TMCW and MMCW soils in growing season were 0.635 and 0.687 gN/m2, and the denitrification gaseous lost amounts were 0.617 and 0.405 gN/m2, respectively. In plant subsystem, the N was mainly stored in root and litter. Soil organic N was the main N storage of the two plant-soil systems and the proportions of it were 93.98% and 92.16%, respectively. The calculation results of N turnovers among compartments of TMCW and MMCW showed that the uptake amounts of root were 23.02 and 28.18 gN/(m2·a) and the values of aboveground were 11.31 and 6.08 gN/(m2·a), the re-translocation amounts from aboveground to root were 5.96 and 2.70 gN/(m2·a), the translocation amounts from aboveground living body to litter were 5.35 and 3.38 gN/(m2·a), the translocation amounts from litter to soil were larger than 1.55 and 3.01 gN/(m2·a), the translocation amounts from root to soil were 14.90 and 13.17 gN/(m2·a), and the soil (0-15cm) N net mineralization amounts were 1.94 and 0.55 gN/(m2·a), respectively. The study of N balance indicated that the two plant-soil systems might be situated in the status of lacking N, and the status might induce the degradation of C. angustifolia wetland.