重金属对秀丽隐杆线虫繁殖的影响

为了探究重金属单独及联合暴露对秀丽隐杆线虫(Caenorhabditis elegans)繁殖的影响及其作用机制,采用96孔板液相暴露试验,以环境相关浓度(0.1~50.0 μg/L)的Cd、Hg、Pb暴露同步化处理秀丽隐杆线虫,24 h后统计其怀卵数及阴门畸形率,以及连续记录72 h内子一代秀丽隐杆线虫的个体数,最后利用2×2析因设计方差分析阐明重金属的两两联合作用模式. 结果表明:与对照组相比,Cd、Hg、Pb单独及联合暴露对秀丽隐杆线虫的繁殖具有显著抑制作用,ρ(Cd)为50.0 μg/L、ρ(Hg)为10.0 μg/L、ρ(Pb)为50.0 μg/L暴露组秀丽隐杆线虫子一代数量分别降低了43.5%、33.8%、51.0%;Cd-Hg暴露组〔当ρ(Cd)、ρ(Hg)分别为50.0、10.0 μg/L时〕、Hg-Pb暴露组〔当ρ(Hg)、ρ(Pb)分别为10.0、50.0 μg/L时〕、Cd-Pb暴露组〔当ρ(Cd)、ρ(Pb)分别为50.0、50.0 μg/L时〕秀丽隐杆线虫子一代个体数分别降低了44.7%、61.0%、53.3%. 进一步研究发现,Cd、Hg、Pb单独及联合暴露会引起秀丽隐杆线虫子宫内受精卵数量降低以及产卵器阴门结构畸形率升高. 2×2析因设计方差分析结果发现,Cd、Hg、Pb两两联合暴露对秀丽隐杆线虫的繁殖表现为没有交互作用或者交互方式为拮抗. 研究显示,秀丽隐杆线虫子宫内怀卵数的降低是其子一代数量显著减少的主要原因,而阴门结构的损伤可能使产卵行为受损,从而进一步加剧重金属对秀丽隐杆线虫繁殖的抑制作用.      

节水灌溉措施下湘东北丘陵林-稻汇水区复合系统铅的迁移

铅通过食物链的迁移和积累对人类健康的毒害作用日益为社会所重视,而水稻是人类铅摄入的主要途径之一,因此,对稻田土壤铅的迁入途径及其过程特征的研究十分必要.为了探明湖南地区远离城镇、工矿区的丘陵稻区铅的输入、迁移、滞留机制,选择位于湘东北地域的汩罗市桃林林场的林地-山塘-稻田汇水区系统作为研究对象,在水稻大田生长期间,原位研究其大气沉降、岗地径流、山塘水、稻田水、水稻生长等过程的铅通量.结果表明：①输入系统的铅源是大气沉降,其中,在水稻生育前期通过东南季风输入的区域外源铅占90%;②山塘是大气沉降铅的主要集纳地貌单元,存留了大气沉降输入岗地和山塘总铅的66%;③林-稻汇水区系统岗地铅净留存28.8~57.7 g·hm^-2,山塘铅净留存604.3~961.9 g·hm^-2,稻田铅净留存89.6~90.9 g·hm^-2;而对照系统岗地铅净输出173.3 g·hm^-2,山塘净留存3427.6 g·hm^-2,稻田净留存87.1 g·hm^-2;④岗地和山塘对铅的截留量能够互补;⑤从岗地通过径流-山塘水过程迁移到稻田的大分子有机物能够增强稻田对铅的截留.综上所述,丘陵林-稻汇水区系统中铅的循环与大气沉降有关,系统内岗地森林类型、郁闭度、降水产流及泥沙、有机物的输出都会影响铅在系统中的迁移和分配.     

L-半胱氨酸改性甲壳素处理含铅、镉工业废水

研究了L 半胱氨酸改性甲壳素作为吸附剂对Pb2 + 、Cd2 + 的动态吸附性能 ,同时考察了流速、溶液中离子的含量、吸附剂的相对用量等因素对吸附效果的影响 ,以及洗脱液的种类和酸度、洗脱速度、洗脱液体积等因素对解吸率的影响。结果表明 ,用该吸附剂填装的吸附柱对含Pb2 + 、Cd2 + 工业废水直接进行处理 ,处理后的水达到了排放标准。     

Radium and radium-daughter nuclides in carbonates: a brief overview of strategies for determining chronologies

Radium isotopes have been used extensively to trace the movement of groundwater as well as oceanic water masses, but these radionuclides (and their daughters) are also useful chronometers for the determination of the time scales of other Earth and environmental processes. The purpose of this overview is to present the application of Ra and Ra daughters in the dating of carbonates. We show that the choice of dating method (decay of excess radionuclide or ingrowth of daughter) depends strongly on the parent/daughter activity ratios in the water in which the carbonate was precipitated. Thus freshly precipitated carbonates uniformly show excesses of ²²⁶Ra relative to its parent ²³⁰Th, and ²²⁶Ra decay can provide ages of carbonates over Holocene time scales. In contrast, carbonates are precipitated in waters of greatly varying ²¹⁰Pb/²²⁶Ra. Corals, deep-sea hydrothermal vent clams and the shelled cephalopod Nautilus live in waters with significant dissolved ²¹⁰Pb and all show excesses of ²¹⁰Pb in their carbonate. Bivalve molluscs from nearshore and coastal waters, and carbonates deposited from groundwater environments (e.g. travertines) in which ²¹⁰Pb is efficiently scavenged from solution, show deficiencies of ²¹⁰Pb relative to ²²⁶Ra. In contrast, fish otoliths strongly discriminate against ²¹⁰Pb regardless of the environment in which the fish lives. Deficiencies of ²²⁸Th relative to ²²⁸Ra are common in all carbonates. Useful time ranges for the ²¹⁰Pb/²²⁶Ra and ²²⁸Th/²²⁸Ra chronometers are ∼100 y and ∼10 y, respectively.     

Distribution of radionuclides in the guano sediments of Xisha Islands, South China Sea and its implication

Several natural and anthropogenic radionuclides (²¹⁰Pb, ²²⁶Ra and ¹³⁷Cs) in guano-phosphatic coral sediments and pure guano particles collected from Ganquan, Guangjin, Jinqing and Jinyin Islands of the Xisha archipelago, South China Sea, were analyzed. The Constant Initial Concentration (CIC) model and the Constant Rate of Supply (CRS) model were applied for age calculation. The average supply rate of ²¹⁰Pb was 126 Bq m⁻² a⁻¹, very close to the flux of northern hemisphere average (125 Bq m⁻² a⁻¹). The activities of anthropogenic radionuclides in the sediments were very low, indicating that human nuclear tests did not notably impact this region. The main source of radionuclides in the sediments was from atmospheric precipitation, and the organic matter derived from plant and produced by nutrient-rich guano could further enhance them.     

Mechanism of lead immobilization by oxalic acid-activated phosphate rocks

Lead (Pb) chemical fixation is an important environmental aspect for human health. Phosphate rocks (PRs) were utilized as an adsorbent to remove Pb from aqueous solution. Raw PRs and oxalic acid-activated PRs (APRs) were used to investigate the effect of chemical modification on the Pb-binding capacity in the pH range 2.0-5.0. The Pb adsorption rate of all treatments above pH 3.0 reached 90%. The Pb binding on PRs and APRs was pH-independent, except at pH 2.0 in activated treatments. The X-ray diffraction analysis confirmed that the raw PRs formed cerussite after reacting with the Pb solution, whereas the APRs formed pyromorphite. The Fourier Transform Infrared spectroscopy analysis indicated that carbonate (CO₃^2-) in raw PRs and phosphate (PO₄^3-) groups in APRs played an important role in the Pb-binding process. After adsorption, anomalous block-shaped particles were observed by scanning electron microscopy with energy dispersive spectroscopy. The X-ray photoelectron spectroscopy data further indicated that both chemical and physical reactions occurred during the adsorption process according to the binding energy. Because of lower solubility of pyromorphite compared to cerussite, the APRs are more effective in immobilizing Pb than that of PRs.     

磷基材料对土壤铅稳定化效果及影响因素的Meta分析

磷基材料对土壤Pb有良好的稳定化效果.利用Meta分析法筛选汇总了1997~2022年磷基材料稳定土壤Pb的90篇文献,从土壤性质、稳定化工艺条件和磷基材料类型这3个方面量化分析了磷基材料对土壤Pb的稳定化率、赋存形态转化和对土壤pH的影响.结果表明,从土壤性质来看,土壤碱性越强（pH≥7.5）、土壤ω（Pb）越低（≤500 mg ·kg^-1）和土壤ω（有机质）越高（>0.5%）时,越有利于磷基材料对土壤Pb的稳定化,稳定化率分别为75.21%、34.97%和93.12%.从稳定化工艺条件来看,磷基材料添加量较高（≥10%）、含水率较高（>50%）、养护时间较长（≥30d）和养护温度较高（≥40℃）时,更有利于土壤Pb的稳定化,稳定化率可分别达到80.65%、84.98%、79.39%和41.44%.从磷基材料类型来看,可溶性磷基材料对土壤Pb有很高稳定化率（96.24%）;其使土壤可交换态Pb和碳酸盐结合态Pb向残渣态Pb转化的转化率达到95.93%;可溶性磷基材料多呈酸性,对土壤pH的降低率为7.27%,难溶性磷基材料多呈碱性,对土壤pH的增加率为3.63%.综上,在土壤pH≥7.5、土壤ω（Pb）≤500 mg ·kg^-1、土壤ω（有机质）>0.5%、可溶性磷基材料添加量≥10%、含水率>50%、养护时间≥30 d和养护温度≥40℃时,磷基材料对土壤Pb的稳定化效果较好.可见在实际Pb污染土壤修复过程中,为提高Pb稳定化率,需综合考虑土壤性质、稳定化工艺条件和磷基材料类型等因素的影响.     

煤矸石中铅、铬、镉的溶出性能

以滕南煤田某煤矿风化煤矸石为研究对象,应用主成分分析法分析了煤矸石粒径对Pb,Cr,Cd溶出浓度的影响,应用回归分析法分析了浸溶时间与Pb,Cr,Cd溶出浓度的关系特征。实验结果表明：模拟湿地浸溶条件下,煤矸石中Pb,Cd,Cr溶出浓度均超出或接近Ⅲ类水体水质标准,对水环境存在污染风险;煤矸石粒径对Pb,Cd,Cr溶出浓度存在影响,粒径越小则Pb、Cr、Cd溶出浓度越大,粒径小于8.0 cm的煤矸石浸溶贡献较大。建立了表征Pb,Cr,Cd溶出浓度与浸溶时间对数（以10为底）关系的一元三次多项式回归方程,经检验均具有显著性。     

Interactions between lead(II) ions and dissolved organic matter derived from organic fertilizers incubated in the field

This work was to study composition characteristics and the subsequent effect on the lead (Pb) binding properties of dissolved organic matter (DOM) derived from seaweed-based (SWOF) and chicken manure organic fertilizers (CMOF) during a one-year field incubation experiment using the excitation-emission matrix-parallel factor (EEM-PARAFAC) and two-dimensional correlation spectroscopy (2DCOS) analysis. Results showed that high aromatic and hydrophobic fluorescent substances were enriched in CMOF-derived DOM and SWOF-derived DOM and enhanced over time. And phenolic groups in the fulvic-like substances for SWOF-derived DOM and carboxyl groups in the humic-like substances for CMOF-derived DOM had the fastest responses over time, respectively. Moreover, both non-fluorescent polysaccharides and fluorescent humic-like substances or fulvic-like substances with aromatic (C=C) groups first participated in the binding process of Pb to SWOF-derived DOM on day 0 and 180 during the lead binding process. In contrast, humic-like substances associated with aromatic (C=C) and phenolic groups gave a faster response to Pb binding on day 360. Regarding CMOF-derived DOM, the fulvic-like substances associated with aromatic (C=C) and carboxylic groups displayed a faster response to Pb ions on day 0. Nonetheless, polysaccharides and humic-like associated with phenolic groups had a faster response on days 180 and 360. It is noteworthy that the polysaccharides, which participated in Pb binding to CMOF-derived DOM, posed a higher risk of Pb in the environment after 360 days. Therefore, these findings gave new insights into the long-term applications of commercial organic fertilizers for the amendment of soil.     

MnO2@Fe3O4/石墨烯复合材料对水中Pb(Ⅱ)的吸附

以氧化石墨烯（GO）为原料制备MnO₂@Fe₃O₄/石墨烯（RGO）,考察吸附过程中MnO₂@Fe₃O₄/RGO投加量、溶液pH值、初始浓度和吸附时间等因素对Pb（Ⅱ）的去除率和吸附量的影响,并运用BET比表面积测试法计算MnO₂@Fe₃O₄/RGO的比表面积和平均孔径,采用扫描电子显微镜（SEM）,振动样品磁强计（VSM）,X射线衍射（XRD）和X射线光电子能谱（XPS）等对样品进行表征.结果表明：MnO₂@Fe₃O₄/RGO的比表面积为89.164m²/g,孔容为0.284cm³/g;随着pH值在2~10范围内增加,复合材料对Pb（Ⅱ）的去除率先增大后减小,pH=6时达到最大值.通过4种等温吸附模型（Langmuir、Freundlich、Temkin、D-R模型）和4种吸附动力学模型（伪一级动力学、伪二级动力学、Elovich、颗粒内扩散模型）拟合发现,MnO₂@Fe₃O₄/RGO对Pb（Ⅱ）吸附符合伪二级动力学模型.吸附等温线更符合Langmiur模型,属于典型的单分子层吸附,以化学吸附为主,最大吸附量为265.3mg/g.