长江经济带突发水污染风险分区研究

长江经济带突发水污染事件频发,对区域人群健康和生态安全造成严峻挑战.环境风险分区是环境风险管理的基础和有效工具.本研究以2015年为基准年,基于环境统计数据、DEM数据、水质监测断面数据和基础地理数据,综合考虑了水系流向、水系级别及水质等因素,以1 km×1 km的网格为基本单元,对长江经济带开展突发水污染风险分区.结果表明:①高风险区面积为3348.9 km~2,占评估区总面积的0.16%;较高风险区面积为26030.7 km~2,占比1.27%;中风险区面积为97971.1 km~2,占比4.79%;低风险区面积为1916838.7 km~2,占比93.77%;②从沿长江干流两岸分布来看,高风险区面积沿长江上游至下游呈逐渐增加趋势,主要集中分布在重庆市中部、湖北省东部、安徽省东部、江苏省中西部、浙江省北部、上海市西部等地;③从沿长江主要支流两岸分布来看,高风险区主要分布在嘉陵江南段、乌江南段、汉水东段、湘江北段、赣江北段等.研究结果可为长江经济带生态环境管理提供科学依据.     

Ozone pollution characteristics and sensitivity analysis using an observation-based model in Nanjing, Yangtze River Delta Region of China

Ground-level ozone (O₃) has become a critical pollutant impeding air quality improvement in Yangtze River Delta region of China. In this study, we present O₃ pollution characteristics based on one-year online measurements during 2016 at an urban site in Nanjing, Jiangsu Province. Then, the sensitivity of O₃ to its precursors during 2 O₃ pollution episodes in August was analyzed using a box model based on observation (OBM). The relative incremental reactivity (RIR) of hydrocarbons was larger than other precursors, suggesting that hydrocarbons played the dominant role in O₃ formation. The RIR values for NO_X ranged from –0.41%/% to 0.19%/%. The O₃ sensitivity was also analyzed based on relationship of simulated O₃ production rates with reductions of VOC and NO_X derived from scenario analyses. Simulation results illustrate that O₃ formation was between VOCs-limited and transition regime. Xylenes and light alkenes were found to be key species in O₃ formation according to RIR values, and their sources were determined using the Positive Matrix Factorization (PMF) model. Paints and solvent use was the largest contributor to xylenes (54%), while petrochemical industry was the most important source to propene (82%). Discussions on VOCs and NO_X reduction schemes suggest that the 5% O₃ control goal can be achieved by reducing VOCs by 20%. To obtain 10% O₃ control goal, VOCs need to be reduced by 30% with VOCs/NO_X larger than 3:1.     

基于生态系统服务供需关系的广西县域国土生态修复空间分区

国土生态修复是我国土地整治战略发展的需求,其空间分区与管控是实施国土整治与生态修复差别化建设的前提条件。以广西各县市为研究单元,在测算和分析生态系统服务供给量和需求量基础上,利用象限匹配法、双变量局部空间自相关和供需协调度来定量分析生态系统服务供需匹配关系、空间聚集程度和协调关联性,进而探讨和划分广西国土生态修复的空间分区及其管控措施与建议。研究表明：（1）广西各县市生态系统服务供给和需求差异明显。环绕广西的四周山林地和重点生态功能区县生态系统服务供给量较高,大中城市区则较低。生态系统服务需求量自东南向西北逐渐减少。（2）广西生态系统服务供需空间匹配呈现高供高需型、低供高需型、低供低需型、高供低需型四种类型,供需局部空间自相关以高-低或低-高的空间聚集为主,且生态系统服务供需协调度平均值为0.531,处于一般均衡。（3）结合生态系统服务供需匹配四类特征和广西地理环境条件,将广西各县域划分为10个分区,并针对各分区提出差异化整治措施和建议。总体上,生态系统服务高供高需型的区域应以保育为主、培育为辅,防止过度开发;高供低需型的区域以保护为主,提高管理水平;低供高需型的区域应以综合改良为主,提高土地效益;低供低需型的区域应以国土生态重构或重建为主,侧重恢复生态系统。     

祁连山七一冰川物质平衡的时空变化特征

基于2011-2016年七一冰川的野外观测资料,结合气象站数据及1975-2015年的遥感影像,分析了冰川末端变化、物质平衡时空变化特征及其对气候变化的敏感性,结果表明：1975年以来,七一冰川末端持续退缩235 m,平均退缩速率为5.9 m/a,冰川面积减少0.13 km²（4.5%）。2011-2016年,七一冰川的平均物质平衡为-476 mm w.e.,平均ELA为4941 m a.s.l.,物质平衡梯度为2.9 mm/m。从季节变化看,受风吹雪和冰面升华影响,11月至次年3月冰川呈负平衡;4月和9月物质平衡受降水控制,随海拔变化呈现降水效应;强消融期（6-8月）物质平衡随海拔升高线性增加;消融期末由9月初延后至9月底。敏感性分析结果表明,物质平衡对气温变化的敏感性为-178.7 mm w.e. °C^-1 a^-1,对降水变化的敏感性为+2.93 mm w.e. mm^-1 a^-1。即61 mm的降水增加才能弥补暖季气温升高1 °C引起的冰川净物质损失。     

Analysing the sensitivity behaviour of two hydrology models

Recently, the New Morris Method has been presented as an effective sensitivity analysis tool for mathematical models. The New Morris Method estimates the sensitivity of an output parameter to a given set of input parameters (first-order effects) and the extent these parameters interact with each other (second-order effects). This method requires the specification of two parameters (runs and resolution) that control the sampling of the output parameter to determine its sensitivity to various inputs. The criteria for these parameters have been set on the analysis of a well-behaved analytical function (see Cropp and Braddock, Reliab. Eng. Syst. Saf. 78:77–83, 2002), which may not be applicable to other physical models that describe complex processes. This paper will investigate the appropriateness of the criteria from (Cropp and Braddock, 2002) and hence the effectiveness of the New Morris Method to determine the sensitivity behaviour of two hydrologic models: the Soil Erosion and Deposition System and Griffith University Representation of Urban Hydrology. In the first case, this paper will separately analyse the sensitivity of an output parameter on a set of input parameters (first- and second-order effects) for each model and discuss the physical meaning of these sensitivities. This will be followed by an investigation into the sampling criteria by exploring the convergence of the sensitivity behaviour for each model as the sampling of the parameter space is increased. By comparing these trends to the convergence behaviour from Cropp and Braddock (2002), we will determine how well the New Morris Method estimates the sensitivity for each model and whether the sampling criteria are appropriate for these models. It will be shown that the New Morris Method can provide additional insight into the functioning of these models, and that, under a different metric, the sensitivity behaviour of these models does converge confirming the sampling criteria set by Cropp and Braddock.     

锑的淡水水质基准及其对我国水质标准的启示

针对我国锑水生生物水质基准缺乏的问题，收集筛选了锑对淡水水生生物的急性和慢性毒性数据，使用评价因子法、毒性百分数排序法和物种敏感度分布法分别推导我国锑的淡水水质基准，通过综合分析和比较，选择物种敏感度分布法推导的急性和慢性的水质基准值（466.62μg/L和88.71μg/L）作为最终的基准推荐值.通过与国内外现有锑相关水质标准进行比较，提出在我国相关水质标准修订中分别制定保护水生生物和人体健康水质标准的建议，避免水质标准对水生生物的"过保护"问题.     

管式反应器石灰雾液脱硫的数学模拟

建立的一维管式反应器雾液脱硫模型是对蒸发和吸收过程的耦合，以膜理论为基础的吸收机理同时考虑了含硫组分的离解、扩散、反应和固体颗粒的溶解。参数敏感性分析表明，对系统脱硫率影响最显的是出口干湿球温差，石灰颗粒粒度和入口ＳＯ２浓度、传质过程的分析表明，反应开始阶段液膜扩散和固体溶解阻力均存在，而气膜扩散在整个反应过程中都起着重要作用。     

灾害区划研究的现状,存在问题与发展趋势

着重分析了灾害区划的现状、存在问题和发展趋势，对灾害区划的目标、原理、方法、类型及指标体系进行了深入探讨。     

昆明-楚雄-大理-丽江地区地震软风险区划实例

应用云南省昆明市、楚雄州、大理州、丽江市1900—2000年这100年内M≥5．0的地震记录资料，对该地区的地震灾害软风险区划进行了实例分析。结果表明，软风险区划图是以带有“层”结构的地图形式表述风险评估结果的，而“层”是根据可能性水平来划分的。因此，软风险区划图对分析结果的表述，不仅能对风险分析提供更多的信息，而且能提供风险值可信度的信息，从而使风险图“服务信息”丰富化。     

气候条件变化对棉纤维品质的影响

对棉纤维品质试验的结果分析表明，其长度受气候条件的影响不明显，而比强度和麦克隆值则明显受气候条件的影响。从变异值分析，受气候影响大小顺序是：比强度〉发克隆值〉长度。影响比强度的气候因子主要是日均温、累积降水量和相对湿度，影响麦克隆值的气候因子主要是日均温和累积降水量或夜均温、累积降水量。并确定影响比强度的日均温最低临界值为24．5℃，最适值为26．1℃，铃期累积降水量的最高临界值为109．9mm，最适值为44．6mm，栩对湿度的最高临界值为77．7％，最适值为67．9％。麦克隆值适宜范围的日均温为20．5～24．8℃，累积降水量为108．2～308．2mm。长度适宜范围的最低温度为14．7～20．8℃，相对湿度为84．7％～89．5％。这些因子和指标的确定为建立棉纤维品质的定量模型奠定了基础。