汾渭平原吸收性气溶胶时空演化及潜在源区分析

在绿色发展理念的带动下,全国多地的空气质量逐渐改善,但汾渭平原大气污染程度逐年走高,颗粒物污染尤为严重.利用OMI/Aura OMAERUV L2气溶胶数据集和PM_2.5站点数据,采用空间自相关分析及后向轨迹模型等方法,探索2005~2019年汾渭平原吸收性气溶胶的时空演化过程,揭示其高值极主导类型以及污染物传输路径和潜在源区.结果表明：①2005~2019年汾渭平原吸收性气溶胶指数（absorbing aerosol index,AAI）年均值波动上升,2006、2013和2017年为汾渭平原AAI高值转折点,年均值均大于0.63;西安和临汾AAI空间稳定性较差为高高聚集极点,在15年间高高聚集区域面积增长15.3%,空间分布更加集中,形成由西安和临汾两极相连的条带状分布区域,占区域总面积的24.2%;低低聚集区域面积锐减6.2%,转变为无特征区域.②汾渭平原AAI冬季数值最高、覆盖区域最广,在临汾极和西安极突破0.8,研究区AAI大于0.6的区域占比91.5%,其次为春季（AAI>0.4）、秋季（AAI>0.3）,夏季全境低值.汾渭平原AAI高值受大气扩散条件、气温和降水量变化影响显著.③利用后向轨迹和潜在源贡献模型得出西安极和临汾极污染物的远距离输送气团来自西北方向,近距离输送气团来自偏东和偏南方向,结合源区下垫面类型确定两个远距离沙尘传输源区（西北风源、北风源）、两个碳质源区（东风源和南风源）和一个沙尘和碳质共同作用源区（黄土高原源）.其中西北风源、黄土高原源和南风源对西安极影响显著,东风源和黄土高原源对临汾极影响显著,临汾极虽受一定程度西北风源和北风源沙尘影响,但影响较小,结合CO空间分布和其与AAI相关性系数的空间分布得出,临汾极吸收性气溶胶为碳质主导,西安极为沙尘和碳质共同作用.     

固相萃取气相色谱法测定地表水中有机磷农药

建立了固相萃取(SPE)气相色谱火焰光度(GC-FPD)检测方法,并且检测了地表水中8种有机磷农药,检测限在0.09～0.26μg/L之间,相对标准偏差为3.1%～9.7%(n=8),加标回收率达到61.3%～103.2%,与传统的气相色谱法相比,该方法具有比较高的重现性和选择性,在地表水有机磷农药的测定中具有很好的应用前景.     

邕江流域有机氯农药残留问题的初步研究

采用固相萃取和GC-ECD对邕江流域水体中17种痕量有机氯农药的残留状况进行分析测定,检测结果表明,邕江干流均检出硫酸硫丹,但有机氯农药浓度较低,均未超过现有相关标准。城市内河残留的有机氯农药以六六六为主,主要来自于长期的历史残留,而硫酸硫丹除朝阳溪和相思湖丰水期未检测到外,均普遍检出。方法检出限为1~5ng/L,替代物加标回收率为103.5%~112.0%。     

Environmental monitoring of complex hydrocarbon mixtures in water and soil samples after solid phase microextraction using PVC/MWCNTs nanocomposite fiber

A novel nanocomposite based on incorporation of multiwalled carbon nanotubes (MWCNTs) in polyvinyl chloride (PVC) was prepared. Proposed nanocomposite was coated on stainless steel wire by deep coating. Composition of nanocomposite was optimized based on results of morphological studies using scanning electron microscopy. The best composition (83% MWCNTs:17% PVC) was applied as a solid phase microextraction fiber. Complex mixture of aromatic (BTEX) and aliphatic hydrocarbons (C₅–C₃₄) were selected as model analytes, and performance of proposed fiber in extraction of the studied compounds from water and soil samples was evaluated. Analytical merits of the method for water samples (LODs = 0.10–1.10 ng L⁻¹, r² = 0.9940–0.9994) and for soil samples (LODs = 0.10–0.77 ng kg⁻¹, r² = 0.9946–0.9994) showed excellent characteristics of it in ultra trace determination of petroleum type environmental pollutants. Finally, the method was used for determination of target analytes in river water, industrial effluent and soil samples.     

气质联用分析加硫酸化污泥中的有机酸

分别采用两种前处理方法分离富集加硫酸化污泥中的有机酸.方法一,利用阴离子交换树脂分离富集有机酸,在不洗脱的情况下直接和乙醇进行酯化反应,然后进行气质联用分析;方法二,利用活性炭纤维吸附型固相微萃取(ACF-SPME)的方法,顶空萃取分离后进行气质联用分析.两种方法的分析结果都未检测到酸化污泥中存在短链的有机酸,只检测到个别长链的和带苯环结构的有机酸.     

重铬酸钾─三氯化钛法测定水中溶解氧

介绍了三氯化钛（ＴｉＣｌ３）与氧反应，以钨酸钠（Ｎａ２ＷＯ４）作指示剂，用重铬酸钾溶液滴定过剩三氯化钛来测定水中溶解氧的方法。本法与碘量法比较，结果表明方法准确、快速，适合于水样中溶解氧的测定     

望虞河西岸九里河中四种除草剂的污染现状

基于气相色谱-质谱联用(GC-MS)法结合固相萃取(SPE)前处理技术,建立了水中4种除草剂氯草定、阿特拉津、乙草胺和异丙甲草胺残留的分析方法,于2018年春(4、5月)、秋(9、10月)和冬(1、3月)季对太湖流域望虞河西岸九里河水体中4种除草剂的污染现状进行调查分析。结果表明,4种除草剂的加标回收率为71. 2%～108%,RSD均10%,方法检出限为3. 5～6. 0 ng/L。九里河水体中氯草定、阿特拉津、乙草胺和异丙甲草胺4种除草剂质量浓度分别为未检出～0. 025 7,0. 019 1～1. 19,未检出～0. 026 0和未检出～0. 094 3μg/L。4种除草剂中阿特拉津最高值接近《地表水环境质量标准》(GB 3838—2002)限值,其他3种其值较低,氯草定首次在太湖流域水体中检出。     

水中乙醛、丙烯醛和丙烯腈3种测定方法的对比

对比研究了大体积直接进样填充柱气相色谱法、顶空-气相色谱法和吹扫捕集-气相色谱法等3种测定水中乙醛、丙烯醛和丙烯腈的方法.结果表明,大体积直接进样法设备简单,但手动进样耗力费时,且灵敏度低,精密度差,直接水样分析易影响色谱柱和检测器的使用寿命;顶空法稳定性好,线性范围宽,相关性和精密度好,适合较高浓度水样的分析;吹扫捕集法操作简便,峰形好,检出限低,回收率高,适合低浓度水样的分析.顶空法和吹扫捕集法自动化程度高,均适用于大批量样品分析.     

Topsoil organic carbon mineralization and CO2 evolution of three paddy soils from South China and the temperature dependence

Carbon mineralization and its response to climatic warming have been receiving global attention for the last decade. Although the virtual influence of temperature effect is still in great debate, little is known on the mineralization of organic carbon （SOC） of paddy soils of China under warming. SOC mineralization of three major types of China＇s paddy soils is studied through laboratory incubation for 114 d under soil moisture regime of 70% water holding capacity at 20℃ and 25℃ respectively. The carbon that mineralized as CO2 evolved was measured every day in the first 32 d and every two days in the following days. Carbon mineralized during the 114 d incubation ranged from 3.51 to 9.22 mg CO2-C/gC at 20℃ and from 4.24 to 11.35 mg CO2-C/gC at 25℃ respectively; and a mineralizable C pool in the range of 0.24 to 0.59 gC/kg, varying with different soils. The whole course of C mineralization in the 114 d incubation could be divided into three stages of varying rates, representing the three subpools of the total mineralizable C： very actively mineralized C at 1-23 d, actively tnineralized C at 24--74 d and a slowly mineralized pool with low and more or less stabilized C mineralization rate at 75-114 d. The calculated Q10 values ranged from 1.0 to 2.4, varying with the soil types and N status. Neither the total SOC pool nor the labile C pool could account for the total mineralization potential of the soils studied, despite a well correlation of labile C with the shortly and actively mineralized C, which were shown in sensitive response to soil warming. However, the portion of microbial C pool and the soil C/N ratio controlled the C mineralization and the temperature dependence. Therefore, C sequestration may not result in an increase of C mineralization proportionally. The relative control of C bioavailability and microbial metabolic activity on C mineralization with respect to stabilization of sequestered C in the paddy soils of China is to be further studied.     

西藏"一江两河"地区人口空间分布的动态演变

人口分布的空间演变是人口发展过程中在时间和空间上的表现形式,人口的集聚与扩散是诠释区域人口空间分布格局与形态的重要方面.对其研究有助于揭示人口分布现状的本质、理解区域空间结构特征及演变趋势.本研究运用局部空间自相关方法,并结合GIS技术,以县域为基本单元,人口密度为衡量指标,对西藏"一江两河"地区1990-2008年间人口分布空间格局的演变进行了分析.分析结果表明,"一江两河"地区各县市(区)人口总量和密度均有明显增长,人口分布总体上呈现出不断集中的态势.局部自相关分析揭示"一江两河"地区开始显现以拉萨市和日喀则市为中心的两个显著的人口高密度区,显示出该区域人口分布的多中心空间结构特征.对以拉萨市、日喀则市和乃东县为中心的区域密度函数进行拟合.多中心区域密度函数的估计结果显示,"一江两河"地区空间发展正逐步由20世纪90年代单中心(拉萨市城关区)阶段,向目前的多中心向心集聚阶段转变,除拉萨市城关区外,日喀则市和乃东县集聚能力开始显现.