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Cao Feiyan Zhang Xiaorong Hao Chunyu Tiwari Shani Chen Bing 《Environmental science and pollution research international》2021,28(7):8022-8035
Environmental Science and Pollution Research - Light absorption enhancement of black carbon due to the aerosol mixing states is an important parameterization for climate modeling, while emission... 相似文献
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三峡水库香溪河库湾氮磷分布状况及沉积物污染评价 总被引:3,自引:0,他引:3
为了解三峡大坝蓄水完成之后香溪河库湾水体及沉积物中氮、磷的分布状况以及沉积物污染水平,2013年4月对三峡水库香溪河库湾进行调查采样,测定表层水及沉积物中氮磷含量和形态组成。结果表明,香溪河库湾表层水总磷(TP)含量范围为0.20~0.51 mg·L~(-1),总氮(TN)含量范围为0.54~2.25 mg·L~(-1),TP主要由磷酸盐(PO_4~(3-))组成,TN主要由硝酸盐(NO_3~-)以及氨氮(NH_4~+)组成,TP在空间上呈现从河口向库尾逐渐升高的分布格局,TN分布从河口向库尾逐渐降低。香溪河库湾沉积物中TP含量变化范围为642~1 189 mg·kg~(-1),TN含量变化范围为867~1 718 mg·kg~(-1),沉积物TP含量分布呈现上游高下游低,沉积物TN分布趋势呈现中间高,两头低。沉积物中TP主要由无机磷(IP)组成,有机磷(OP)所占比例较小,其中IP由钙磷(Ca-P)、铁铝磷(Fe/Al-P)组成,三者含量:Ca-POPFe/Al-P,且沉积物TP含量空间变化受到三者影响(P0.05)。采用单一因子标准指数法对香溪河库湾沉积物中TN、TP污染水平进行评价,结果表明,表层沉积物中TN、TP最低级别污染指数平均值为2.0和1.6,表层沉积物中TN、TP污染指数均超过最低污染水平,且TP的严重级别污染指数达到0.5以上。三峡水库三期蓄水完成以后,香溪河库湾表层水体中氮磷含量较初期蓄水有所升高,各样点沉积物中氮磷含量表现出相同的趋势,沉积物中不稳定磷释放对水体富营养化具有影响,香溪河库湾的表层沉积物已经受到一定的污染,磷污染水平较高。 相似文献
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Li Yuxin Zhong Mingqing He Xianzhi Zhang Ruoyu Fu Yu You Ruolan Tao Feiyan Fang Lei Li Yuanyuan Zhai Qingfeng 《Environmental science and pollution research international》2023,30(9):22176-22187
Environmental Science and Pollution Research - Titanium nanoparticles and pyrethroid pesticides are now being widely used in industrial, agriculture, and biomedical applications. In recent years,... 相似文献
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文章运用主成分分析法与熵值法相结合的方法,以公众参与环境治理的各个途径为数据依据,先通过数学变换和降维得到新的指标并算出分值,再通过熵值法赋权,对31个省市的公众参与水平进行评价。结果表明,华东地区公众参与水平最高,后依次是中南、西南、东北和华北地区。以此结果为基础提出制定个性化环保政策、提升政府环境治理能力和提升公众环保意识3条建议。 相似文献
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Chen F Yang Q Pehkonen SO Ray MB 《Journal of the Air & Waste Management Association (1995)》2004,54(10):1281-1292
The relationship between the irradiance in a photoreactor and the rate of photodegradation of organics is essential in the scaling-up of photoreactors to treat large volumes of air contaminated with organic pollutants. In this study, the analysis is adopted to compare results obtained from two different photoreactors. Initially, the applicability of two light models in calculating the irradiance in two photoreactors was evaluated. Thereafter, kinetic models of ultraviolet (UV) photooxidation of chloroform (CHCl3) and carbon tetrachloride (CCl4) from the archived literature were tested using experimental data under various operating conditions and different irradiances. Sensitivity analyses were conducted using different values of model parameters to determine the significance of each parameter on the photodegradation of the two chlorinated organics. For compounds that undergo photolysis as a primary mode of degradation, the rate of photodegradation at low initial concentrations can be predicted easily by the following equation: d[C]/dt = -2.303Iave, lambdaepsilonlambdaphilambda[C]. Although the photodegradation of chlorinated organic compounds in dry and humid air can be predicted well, it is difficult to predict the Cl* sensitized oxidation occurring at high initial concentrations. A good agreement between the simulated and experimental data provides a sound basis for the design of large-scale reactors. 相似文献
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以云贵高原岩溶深水水库——万峰湖为例,于2016年9月对该水库水体进行连续走航观测及分层采样,测定水体温度(T)、酸碱度(pH)、电导率(Cond)、总溶解固体物(TDS)、氧化还原电位(ORP)及碱度(ALK),通过水化学平衡原理及亨利定律计算水体二氧化碳分压(pCO_2).结果表明:干流表层pCO_2为128.84~222.51 Pa,均值为184.03 Pa;支流表层pCO_2为140.32~285.00 Pa,均值为216.78 Pa.剖面上,干流pCO_2为128.84~1076.81 Pa;支流pCO_2为140.32~657.23 Pa,干、支流剖面pCO_2随水深度增加而升高.TDS浓度为203.0~286.7 mg·L-1,溶解无机碳(DIC)浓度为2.56~3.37 mmol·L-1.相关分析表明:水体pCO_2与ORP呈显著正相关,分析认为受水生生物作用影响,水生生物消耗表层溶解CO2使表层水体pCO_2较低.同时,pCO_2与TDS、DIC呈正相关,说明万峰湖流域内溶蚀作用控制的河流碳酸盐体系是影响水体pCO_2的主要原因.干、支流水体pCO_2处于过饱和状态,成为大气CO2的源.根据Wanninkhof提出的淡水水-气界面交换系数的通量模式,估算干、支流水-气界面CO2交换速率分别为0.16、0.19μmol·m-2·s-1,其扩散通量干流为9.77~20.84 mmol·m-2·d-1,均通量为15.30 mmol·m-2·d-1;支流为11.55~27.88 mmol·m-2·d-1,均通量为19.72 mmol·m-2·d-1.与世界其它河流、水库相比较,水库干、支流二氧化碳扩散通量比热带地区河流Amazon、Curua-Una、Tucurui小;与温带地区黄河相比,扩散通量要大;与亚热带岩溶区水库相比差异不明显. 相似文献