基于因子分析定权法的丹江口水库水体营养度综合评价

指标权重值的确定是多指标水质评价法实际应用中的关键问题。针对模糊评价等方法中权重值确定所具有的主观性,提出了基于因子分析定权的水质综合评价法及富营养化指数的概念,并将其应用于南水北调中线工程水源地-丹江口水库水体营养度的综合评价。结果表明,丹江口库区的污染物类型可以分为两类;丹江口库区水体营养度全年时段内均处于中营养化水平,但是,不同采样点、不同季节时的水体富营养化指数的差异还是较大的。总体来看,丹江口库区中,小太平洋水质最好,陶岔水质次之,大石桥水质最差。     

黄渤海气溶胶光学厚度的多源卫星遥感产品精度分析和时空分布特征研究

以黄渤海上空大气为目标研究区,基于AERONET观测网,获取该区域2015—2017年的气溶胶光学厚度（AOD）实测数据,并对可见红外成像辐射计VⅡRS,中分辨率成像光谱仪MODIS,静止水色卫星成像仪GOCI与新一代地球同步气象卫星AHI H8的AOD遥感产品展开精度验证.同时,利用长时间的遥感影像探究并分析AOD在不同时空尺度下的分布特征与变化情况.结果表明：同其它AOD遥感产品相比,GOCI AOD展示出了高采样频率及高精度的特性.此外,在研究区域AOD的逐小时遥感影像中未发现明显的变化规律,而月平均图则显示出从黄渤海西部至中部再到东部AOD逐渐递减的趋势,且该趋势在研究区域不同的地方是具有差异的.不仅如此,本文还尝试分析影响AOD反演精度的潜在因子,发现其可能与地表反射率提取的准确度与预设气溶胶模型设置的合理性有关.     

Remote sensing estimation of colored dissolved organic matter (CDOM) from GOCI measurements in the Bohai Sea and Yellow Sea

Environmental Science and Pollution Research - Colored dissolved organic matter (CDOM) is the main constituent of dissolved organic matter (DOM), also a key indicator of water quality conditions....     

利用土地人口容力开放模型对沪苏锡常城市群的分析

本文提出了土地人口容力,即单位面积土地的人口容量的概念,建立了描述和测算开放区域人口容力的模型,确立了模型对多种人口容力定义,揭示了不同人口容力模型的内在联系性,并将它用于沪苏锡常城市群的土地人口容力测算和分析。     

Contamination levels and human health risk assessment of toxic heavy metals in street dust in an industrial city in Northwest China

This study investigated the content, distribution, and contamination levels of toxic metals (Cd, Cr, Cu, Pb, and Zn) in street dust in Lanzhou, an industrial city in Northwest China. Meanwhile, the risk these metals posed to the urban ecosystem and human health was also evaluated using the potential ecological risk index and human exposure model. Results showed that concentrations of these metals in the dust are higher than the background value of local soil, with Cu having the highest levels. The districts of Anning and Xigu had the most extreme levels of contamination, while Chengguan and Qilihe districts were lightly contaminated, which can be partly attributed to human activities and traffic densities. In comparison with the concentrations of selected metals in other cities, the concentrations of heavy metals in Lanzhou were generally at moderate or low levels. Heavy metal concentration increased with decreasing dust particle size. The pollution indices of Cr, Cd, Cu, Pb, and Zn were in the range of 0.289–2.09, 0.332–2.15, 1.38–6.21, 0.358–2.59, and 0.560–1.83 with a mean of 1.37, 1.49, 3.18, 1.48, and 0.897, respectively. The geo-accumulation index (I _geo) suggested that Zn in street dust was of geologic origin, while Cd, Cr, Pb, and Cu were significantly impacted by anthropogenic sources. The comprehensive pollution index showed that urban dust poses a high potential ecological risk in Lanzhou. Non-carcinogenic and carcinogenic effects due to exposure to urban street dust were assessed for both children and adults. For non-carcinogenic effects, ingestion appeared to be the main route of exposure to dust particles and thus posed a higher health risk to both children and adults for all metals, followed by dermal contact. Hazard index values for all studied metals were lower than the safe level of 1, and Cr exhibited the highest risk value (0.249) for children, suggesting that the overall risk from exposure to multiple metals in dust is low. The carcinogenic risk for Cd and Cr was all below the acceptable level (< 10⁻⁶).

     

Synthesis and applications of carbon quantum dots derived from biomass waste: a review

Environmental Chemistry Letters - In the context of the circular economy and decreasing earth resources, waste should be converted into value-added materials such as carbon quantum dots, which are...     

乌梁素海表层沉积物重金属分布特征及生态风险评价

采样分析了内蒙古乌梁素海表层沉积物中Cu、Zn、Pb、Cr、Cd、Hg和As的含量、分布特征和富集状况,分别以现代工业化前正常颗粒沉积物中重金属含量的最高背景值和河套地区土壤中重金属含量背景值为参照,采用瑞典科学家Lars Hakanson的潜在生态危害指数法对7种重金属的富集系数和生态危害系数以及各采样点的生态危害指数进行了评价。结果表明,乌梁素海表层沉积物中As和Pb的空间变异性较大;以2种背景值为参比得出的重金属污染水平顺序相近,Hg和As为对乌梁素海生态环境具有潜在影响的主要重金属元素;同时表明,以河套地区土壤重金属背景值为参照更能直观地反映出乌梁素海表层沉积物中重金属的污染程度。     

我国西北黄土对阿特拉津的吸附行为及影响因素

为了探讨ATZ(阿特拉津)在黄土中的吸附/解吸行为及主要影响因素,以我国西北黄土为供试土样,采用批量试验法研究了黄土对ATZ的吸附动力学和热力学行为特征. 结果表明:黄土对ATZ的吸附动力学过程更符合准二级动力学模型,吸附热力学过程更符合线性分配的Henry吸附模型(R2>0.90),吸附过程中ΔGθ(吉布斯自由能)及ΔHθ(焓变)均小于0、ΔSθ(熵变)大于0,25～45 ℃温度范围内E(吸附平均自由能)为0.86～1.30 kJ/mol,表明黄土对ATZ的吸附过程以物理吸附为主,属于自发放热过程且导致吸附体系混乱度增加. 黄土对ATZ的吸附影响因素分析结果显示,随着系统温度的升高,ATZ在黄土中的饱和吸附量下降;pH在2～10范围内变化时,ATZ在黄土中的饱和吸附量随pH的增加呈明显降低趋势;初始ρ(ATZ)从2.5 mg/L增至10.0 mg/L时,黄土对ATZ的饱和吸附量也相应地从0.082 5 mg/g增至0.621 0 mg/g. 结果显示,ATZ在黄土中的吸附速率受内部扩散、表面吸附和液膜扩散的共同影响,并且吸附过程主要受到土壤有机质疏水性分配作用的影响.