Global fallout Pu recorded in lacustrine sediments in Lake Hongfeng, SW China

Studies on the distribution and isotope compositions of fallout Pu are important for source characterization of possible future non-fallout Pu contamination in aquatic environments, and useful for dating of recent sediments to understand the pollution history of environmental contaminants. We present the historical record of atmospheric Pu fallout reconstructed from a sediment core from Lake Hongfeng, China. The Pu activity profile was in agreement with the 137Cs profile. Inventories were 50.7 Bq m(-2) for 239+240Pu and 1586 Bq m(-2) for 137Cs. The average 240Pu/239Pu atom ratio was 0.185+/-0.009, indicating that Pu originated from global stratospheric fallout rather than from direct tropospheric or close-in fallout from the Chinese nuclear testing conducted in the 1970s. Our data suggested that Lake Hongfeng would be an ideal setting for monitoring atmospheric fallout and environmental changes in this region.     

煤层透气性系数的优化和简化计算方法

煤层透气性系数是用以考察保护层开采效果和设计瓦斯抽采系统的重要参数之一,钻孔径向流量法是求取该系数最常用的算法。利用理论推导和图形分析方法,探讨流量准数、时间准数、煤层透气性系数与参数A,B间的关系。在此基础上,针对科研工作和现场管理的实际情况,提出求解透气性系数的2种新算法及其算法流程,并对时间准数-参数A,B函数关系中的间断点问题进行讨论和分析,解决此区间内求解透气性系数相应计算公式等问题。理论和实例分析表明:算法1在不更改最终计算公式和结果的前提下,省去了繁琐的试算过程,既保证了可靠性也优化了计算流程;算法2以稍减精度的代价对计算流程进行进一步的简化,其结果仍有较高精度。     

峡山地不同垂直带土壤层的水文功能及其影响因子

渗透性能和持水能力是土壤重要的水力学性质，是土壤调节径流、保持水土和涵养水源等水文功能的基础。以三峡库首的夷陵-大老岭山地为对象，采集亚高山棕壤针叶林地、中山黄棕壤针阔混交林与茶园地和低山黄壤针叶林地等4个样点剖面的土壤样品，在室内进行土壤饱和导水率、水分特征曲线和理化性质测定，量化了不同样地土壤渗透性能、持水能力和水分库容等水文功能参数，并明确了其主要影响因子。结果表明: 研究区山地土壤饱和导水率在0.06～14.78 mm/min之间，亚高山棕壤和中山黄棕壤林地土壤渗透性能较好，其平均饱和导水率在7.15～14.78 mm/ min之间，低山黄壤次之（1.3 9 mm/min），中山黄棕壤茶园土壤渗透能力最差（1.17 mm/min）。不同类型土壤的饱和含水量、毛管含水量、田间持水量存在较大差异，凋萎含水量差异较小。同一类型土壤的不同发生层内，土壤饱和含水量随土壤深度的增加而递减，毛管持水量和田间持水量随土层深度的增加波动上升。不同样地间土壤水分总库容差异较大，随着海拔的升高，土壤水分总库容增加。土壤水分特征参数与土壤性质的相关分析表明，饱和导水率与土壤总孔隙度呈显著正相关，与容重呈显著负相关；饱和含水量、毛管持水量、田间持水量均与土壤总孔隙度、粘粒含量呈显著性正相关，与容重呈显著负相关；饱和含水量与根系重量呈显著正相关；毛管持水量、田间持水量与砂粒含量呈显著负相关。与中山茶园地和低山黄壤林地相比，亚高山棕壤和中山黄棕壤林地渗透性能较好且持水性更强，具有更好的调蓄径流和涵养水源的水文功能。 关键词： 山地土壤；土壤孔隙度；饱和导水率；持水能力；三峡库区     

三峡水库蓄水期不同调度方案对洞庭湖出口水位的影响

洞庭湖水情受到长江和四水的综合影响，因此三峡水库蓄水运行必将对洞庭湖出口水位产生影响。通过构建模型对洞庭湖出口的水位过程进行模拟，以三峡出库日均流量、洞庭湖四水合成日均流量为输入，城陵矶站日水位过程为输出，以量化和分析城陵矶水位变化受三峡水库调度的影响。通过三峡入库流量代替出库流量，还原自然状态下的水位过程，并根据各调度方案计算的出库流量模拟各调度方案下城陵矶的水位变化过程。对比各调度方案下三峡水库蓄泄水对洞庭湖出口水位的影响可以发现：各蓄水方案对洞庭湖出口水位都造成了一定的影响，起蓄时间较早的方案影响时间较长，整体上平均水位变化也较大，但起蓄后水位变化较为平缓；起蓄时间较晚的方案影响时间较短，整体上平均水位变化相对较小，但起蓄后水位变化较为剧烈。考虑到不同年份和不同来水类型情况对洞庭湖出口水位的影响存在差异，各蓄水方案的优劣需要具体分析和讨论     

Comparisons of three plant species in accumulating polycyclic aromatic hydrocarbons (PAHs) from the atmosphere: a review

Environmental Science and Pollution Research - Plant leaves play a key role in the accumulation of PAHs, as they are able to capture PAHs from the air. In this paper, the mechanism, including...     

环境中的微塑料:赋存、检测及其危害

近年来，由个人护理品及废旧塑料直接或间接产生的微塑料不断地在各种环境介质中被检出，且微塑料会对生态系统产生各种危害，因此对微塑料的研究受到越来越广泛的关注。阐述了微塑料在水体、沉积物、沙滩和生物体中的赋存情况，介绍了微塑料的采集与分离方法，以及定性与定量分析方法。指出微塑料对环境及生物体产生的危害，提出现阶段研究存在的主要问题，并对今后的研究方向进行了展望。     

发酵鸡粪和有机磷肥对土壤中Pb、Cd污染的影响

研究了湘西地区常用的发酵鸡粪和有机磷肥施用对不同程度Pb、Cd复合污染土壤中乙三胺五醋酸(DTPA)提取态Pb(DTPA-Pb)、DTPA提取态Cd(DTPA-Cd)和土壤酶的影响,并研究了对于种植黑麦草(Lolium perenne L.)的影响。结果表明:(1)施用发酵鸡粪和有机磷肥均能显著改善土壤酸性,一定程度上提高土壤有机质含量。在加入质量浓度200mg/kg总Pb、2mg/kg总Cd复合污染土壤中施用有机磷肥,能有效钝化土壤DTPA-Pb、DTPA-Cd,但在400mg/kg总Pb、4mg/kg总Cd复合污染土壤中钝化效果有限,其优先钝化DTPA-Pb。施用发酵鸡粪不能有效钝化土壤DTPA-Pb、DTPA-Cd。(2)施用发酵鸡粪和有机磷肥均显著提高黑麦草鲜重。虽然施用有机磷肥能更有效的钝化土壤DTPA-Pb、DTPA-Cd,但对于黑麦草种植而言,施用发酵鸡粪能更有效的降低其对Pb和Cd的积累,并且主要积累到根部。(3)施用发酵鸡粪对土壤碱性磷酸酶活性、脱氢酶活性和脲酶活性有显著的促进作用。综合而言,湘西地区种植牧草黑麦草,施用发酵鸡粪比较合适,能有效改善土壤酸性,提高黑麦草鲜重和土壤酶活性,降低黑麦草对Pb和Cd的积累。     

露天矿山隐伏盲空区精确探测及爆破优化设计

隐伏盲空区是严重威胁露天矿山正常采矿作业的安全隐患,应予以探明并处置。针对露天矿隐伏盲空区探测难度大、崩落处置爆破设计精度差等问题,以白马铁矿1号溜井盲空区为例,首先基于矿山历史资料,利用钻探手段,初步圈定盲空区异常分布范围;然后运用钻孔激光扫描设备进行三维精确扫描,获得盲空区塌腔三维形态和真实边界,并以实测数据为基础,利用逆向建模方法,构建盲空区三维可视化模型;最后根据盲空区的三维空间特征和分布条件,进行爆破分区及参数优化设计。结果表明:采用钻探圈定结合三维激光精确扫描建模的综合探测方法,可获得露天矿山盲空区的可靠信息,准确掌握盲空区垮塌现状,进而为制定更为精准的爆破设计方案提供重要依据,最终达到消除盲空区的目的。研究结果对保障矿山安全生产具有重要意义,同时可为类似工程提供有益参考。     

红壤和磷灰石对沉积物重金属稳定化的影响

利用磷灰石、红壤及两者复配组合对污染沉积物中重金属进行稳定化处理,通过TCLP和改进的BCR连续提取法对稳定化效果进行分析和评价。结果表明,在稳定化试验中,对Cu、Cd和Zn的稳定效果由大到小为红壤+磷灰石、磷灰石、红壤;其中,红壤+磷灰石对Pb的稳定效果与磷灰石单独添加相近,显著大于红壤。5%磷灰石+5%红壤添加3个月后,Cu、Cd、Zn和Pb的稳定效率分别达到59.83%、29.43%、31.00%、96.06%。添加5%磷灰石时,Cu、Cd、Zn和Pb的稳定效率分别为52.46%、24.67%、25.23%、96.06%。红壤的添加不同程度地促进了磷灰石对Cu、Cd和Zn的稳定效率。连续提取试验结果表明.磷灰石单独和复配添加均使Cu、Zn和Pb的生物可利用态和潜在生物可利用态占比降低,生物不可利用态占比增大。5%磷灰石+5%红壤处理中,Cu、Cd、Zn和Ph的生物可利用态和潜在生物可利用态的比例总和分别降低了19.31%、5.11%、20.11%和68.97%。相比磷灰石单独处理,复配处理进一步促进了Cd和Zn的酸溶态向残渣态转化。磷灰石和红壤+磷灰石复配处理能有效降低沉积物中重金属的危害。     

Speciation and fractionation of heavy metals in soil experimentally contaminated with Pb,Cd, Cu and Zn together and effects on soil negative surface charge

Speciation and fractionation of heavy metals in soil subsamples experimentally loaded with Pb, Cd, Cu and Zn in orthogonal design was investigated by sequential extraction, and operationally defined as water-soluble and exchangeable(SE), weakly specific adsorbed( WSA),Fe and Mn oxides-bound(OX) and organic-bound( ORG). The results showed that fractions of heavy metals in the soil subsamples depended on their speciation. About 90% of Cd and 75% of Zn existed in soil subsamples in the SE fraction. Lead and Cu existed in soil subsamples as SE, WSA and OX fractions simultaneously, although SE was still the major fraction. Organic-bound heavy metals were not clearly apparent in all the soil subsamples. The concentration of some heavy metal fractions in soil subsamples showed the good correlation with ionic impulsion of soil, especially for the SE fraction. Continuous saturation of soil subsamples with 0.20 mol/L NH4CI, which is the first step for determination of the negative surface charge of soil by the ion retention method, resulted in desorption of certain heavy metals from the soil. It was found that the percentage desorption of heavy metals from soil subsamples depended greatly on pH, the composition and original heavy metal content of the soil subsamples. However, most of the heavy metals in the soil subsamples were still be retained after multiple saturation. Compared with the parent soil, the negative surface charge of soil subsamples loaded with heavy metals did not show difference significantly from that of the parent one by statistical analysis. Heavy metals existed in the soil subsamples mainly as exchangeable and precipitated simultaneously.