羊八井地热区典型植物对氟的吸附富集特征探究

采用水浴提取法处理羊八井地热区土壤和植物样品中可溶性氟，并用离子选择性电极法测定提取液及地热水中的氟。结果表明，地热水中氟离子最高为162 mg/L，土壤和植物中水溶性氟分别为347 mg/kg~937 mg/kg和189 mg/kg~164 mg/kg。氟离子在不同植物中的分布差异较大，嵩草属植物富集氟离子的能力最强，故可利用植物修复技术对高氟地热水、土壤净化处理，以降低氟污染。     

露天矿溜槽粉尘逸散规律试验研究

为探索露天矿用溜槽系统粉尘逸散的影响因素,阐明溜槽系统运输过程中粉尘的产生机理和运移规律,从而解决溜槽系统产生的粉尘污染问题,以抚顺西露天矿为研究背景,运用相似理论,建立溜槽模型,通过单因素试验和正交试验,分别研究物料粉岩质量分数、物料含水率、溜槽倾角对溜槽运行过程中粉尘质量浓度的影响。单因素试验结果表明,粉尘质量浓度随物料粉岩质量分数、溜槽倾角增大而逐渐增大,随含水率增大而逐渐降低,溜槽底部粉尘质量浓度受影响变化幅度较大,溜槽中部和上部变化较小。溜槽粉尘质量浓度分布规律为溜槽底部粉尘产生量最大,中部次之,上方最小。溜槽底部为粉尘污染防治重点区域。正交试验结果表明,物料含水率对粉尘逸散影响最大,其次是粉岩质量分数,溜槽倾角影响最小。     

CASS工艺在医院污水处理中的应用效果研究

通过采样分析以及考察CASS工艺在徐州某医院污水处理中的实际应用效果情况.结果发现,进水CODG、BOD5、氨氮、TP和总大肠茵群,质量浓度分别为200～300,120～260,7～15,26～3.5 mg/L和大于24000个/L,对应地,出水质量浓度分别为23～65,11～65,0.1～2.8,1.2～1.6 mg/L和小于1000个/L.去除率分别为77.38%～37%,41.73%～54.54%,73.57%～92.78%,66.36%～90.91%和97.08%～99.83%.检测的各项指标除TP外均达到了<污水综合排放标准>中的二级排放标准.针对TP超标问题,并且从CASS工艺除磷的原理及各影响因素方面分析了其超标原因,可能是由于回流污泥中携带的硝酸盐抑制了磷的有效释放.建议利用反硝化除磷原理.将厌氧区设计成1个相对独立的区域,以达到更好的除磷效果,以便为CASS工艺在提出更高的水质要求条件下,依旧能够发挥其作用.     

用于磷吸附的载铁(β-FeOOH)沸石制备及特性简

以天然沸石为载体，采用FeCl₃水解法制备用于磷吸附的载铁沸石（β-FeOOH-Z），优化β-FeOOH-Z的制备条件，包括FeCl₃溶液浓度、负载pH值、负载时间、负载温度和烘干温度，并利用X射线衍射（XRD）和傅里叶变换红外光谱（FTIR）对β-FeOOH-Z及其磷吸附特性进行分析。结果表明，β-FeOOH-Z的优化制备条件为：FeCl₃溶液浓度1 mol/L、负载pH值6、负载时间24 h、负载温度25℃和烘干温度60℃。优化制备条件下，100~120目沸石的载铁量为100.2 mg/g，铁的负载率为18%，其磷吸附量为7.68 mg/g，比天然沸石提高79.6%。XRD分析结果表明，β-FeOOH-Z中的杂质元素较天然沸石减少，并有效负载β-FeOOH；制备条件对β-FeOOH-Z的成分有较大影响，FeCl₃溶液浓度较低、负载温度和烘干温度过高均使β-FeOOH-Z中含有α-Fe₂O₃，并导致其磷吸附效率降低。FTIR分析结果表明，β-FeOOH-Z的表面羟基在其吸附磷过程中起重要作用，羟基与磷酸根离子的配位交换是β-FeOOH-Z吸附磷的主要作用机制。     

煤基腐殖酸对外源砷胁迫下玉米生长及生理性状的影响简

为了筛选用于砷污染土壤治理的煤基腐殖酸，采用盆栽实验研究了施用不同种类和浓度的煤基腐殖酸及EDTA对外源砷胁迫下玉米株高、株鲜重、株干重、根干重、砷积累量、叶片抗氧化酶（POD，SOD和CAT）活性和脯氨酸含量的影响。结果表明，11种供试煤基腐殖酸均促进了玉米生长，提高了叶片POD、SOD和CAT活性。其中6和10号腐殖酸可降低土壤砷活性和显著抑制玉米吸收和积累砷，而8和9号腐殖酸增加了土壤活性砷和显著促进了玉米对砷的吸收和累积，且不同程度地强于EDTA。除8和9号外，其余腐殖酸均可明显降低玉米叶片脯氨酸的含量。EDTA可显著促进玉米吸收和积累砷，且加剧了砷对玉米的危害。因此，8和9号供试煤基腐殖酸可以替代EDTA活化土壤砷，与植物配合以提高砷污染土壤的植物修复速度和效果，而6和10号供试煤基腐殖酸则可用于土壤砷钝化剂，以保证作物产品的安全。     

Combined application of chemical fertilizer with green manure increased the stabilization of organic carbon in the organo-mineral complexes of paddy soil

Environmental Science and Pollution Research - The influence of the combined application of chemical fertilizer with green manure on the stabilization of organic carbon (C) was explored in the...     

Male reproductive toxicity involved in spermatogenesis induced by perfluorooctane sulfonate and perfluorooctanoic acid in Caenorhabditis elegans

Environmental Science and Pollution Research - As a persistent organic pollutant, perfluorooctane sulfonate (PFOS) and perfluorooctanoic acid (PFOA) have gained increasing research attention over...     

Experimental and simulated evaluations of airborne contaminant exposure in a room with a modified localized laminar airflow system

Environmental Science and Pollution Research - The traditional mixing ventilation is not an energy effective approach to remove indoor air pollutants, maintain breath zone air quality, and control...     

Combined effects of nitrogen addition and organic matter manipulation on soil respiration in a Chinese pine forest

The response of soil respiration (Rs) to nitrogen (N) addition is one of the uncertainties in modelling ecosystem carbon (C). We reported on a long-term nitrogen (N) addition experiment using urea (CO(NH₂)₂) fertilizer in which Rs was continuously measured after N addition during the growing season in a Chinese pine forest. Four levels of N addition, i.e. no added N (N0: 0 g N m⁻² year⁻¹), low-N (N1: 5 g N m⁻² year⁻¹), medium-N (N2: 10 g N m⁻² year⁻¹), and high-N (N3: 15 g N m⁻² year⁻¹), and three organic matter treatments, i.e. both aboveground litter and belowground root removal (LRE), only aboveground litter removal (LE), and intact soil (CK), were examined. The Rs was measured continuously for 3 days following each N addition application and was measured approximately 3–5 times during the rest of each month from July to October 2012. N addition inhibited microbial heterotrophic respiration by suppressing soil microbial biomass, but stimulated root respiration and CO₂ release from litter decomposition by increasing either root biomass or microbial biomass. When litter and/or root were removed, the “priming” effect of N addition on the Rs disappeared more quickly than intact soil. This is likely to provide a point of view for why Rs varies so much in response to exogenous N and also has implications for future determination of sampling interval of Rs measurement.