污染物在土壤——植物系统中迁移规律的数学模拟研究：Ⅱ…

论述了大孔隙和优先水流的成因，类型及其对溶质和污染物在土壤中迁移的影响。介绍了优先水流的实验研究方法和数据模型的研究进展。     

气溶胶中正构烷烃的碳优先指数研究

本文研究了北京、广州两地不同季节气溶胶颗粒物上正构烷烃的碳优先指数值(CPI)随季节和颗粒物粒径的变化规律。结果表明,北京地区气溶胶中正构烷烃的CPI值:春>夏>秋>冬;广州地区为冬>春>夏,显示了不同的地区特征,而且随着气溶胶颗粒物粒径的减小,正构烷烃的CPI值亦减小。     

稻田氮、磷损失与过程监测方法研究进展

水稻是我国主要的粮食作物之一。水稻生产过程中土壤和肥料中的部分氮磷元素以溶质或颗粒形态通过淋溶、径流迁移至周围水体,造成地下水污染和水体富营养化。稻田土壤中氨挥发产生的氨气和反硝化反应产生的氧化亚氮气体进入大气,加剧了温室效应。笔者围绕稻田氮磷的气体挥发、径流和淋溶3个流失途径介绍了国内外常用的监测方法,并进一步讨论了针对径流和淋溶这2种流失途径的监测指标、监测频率和监测深度等问题,总结了2种流失途径的主要氮磷流失形态,根据产流特征和施肥时间确定监测时间节点,综合考虑植物吸收和地下水深度确定淋溶监测深度,以期为稻田氮磷流失监测提供相关技术支持和科学依据。     

长江三角洲流域保护水生生物优先控制农药品种筛选

以长江三角洲流域为研究区域,首先明确了以保护水生生物为目标的优先控制农药品种的筛选原则,并以模型预测为基础,根据农药对水生生物的风险性,筛选形成了长江三角洲流域保护水生生物优先控制农药品种名录。名录共包含15种农药有效成分,一方面可为我国地表水农药生态基准的制定提供优先次序,另一方面对于长江三角洲流域地表水体农药污染控制具有重要的指导意义。     

地下水氟污染及其迁移转化模拟试验的初步分析

本文分析了地下水含氟量的变化特征以及氟污染地下水的类型、并通过不同pH值、不同含钙、氟浓度的溶液和工业废水淋溶各种土壤的试验,以初步研究氟在土壤、地下水中迁移、转化的规律。又阐述了我国地方性氟中毒主要分布地带的特征。最后提出了防止氟中毒和地下水氟污染的措施。     

坡地径流与溶质输出研究进展

坡耕地是我国水土流失的重要策源地,也是农业面源污染重要污染源。坡地径流和溶质输出是水土流失及其面源污染的一个重要过程,也是坡地农业生态系统水和物质循环的一个重要过程。坡地水文过程和溶质迁移转化不仅是土壤学近期的重点研究内容,也是需解决的资源环境问题之一。文章从坡地降雨水文过程的地表径流、壤中流和地下径流的输出研究,壤中流模拟研究以及坡地降雨条件下土壤溶质运移模拟等3个方面总结了国内外坡地径流与溶质输出的相关研究结论。同时指出：（1）红壤坡地地表径流、壤中流和地下径流的输出特征及规律还有待进一步研究。（2）对于土壤溶质运移模拟研究,现有成果主要是研究径流和溶质在土壤中的垂向运移,而对其输出过程却很少研究,尤其是坡面径流和土壤溶质分层输出的耦合关系还没有深入的研究。（3）土壤溶质运移理论的研究亟需从封闭的室内土柱试验扩展到野外大田观测,以获取足够的数据资料来确切地描述溶质运移过程,使理论研究与生产实际问题联系得更紧密。（4）同位素方法应用、野外长期定位试验和模拟模型是未来坡地径流与溶质输出研究需加强的几个方面。     

某化工园区场地土壤地下水污染物的分布特征

本研究以长江经济带某典型化工园区为例,探索了该园区土壤与地下水污染的组成特征和分布情况。通过实地调查和采样分析,系统监测了该园区内外土壤与地下水的污染状况,并运用差异分析、相关性分析等,评估了污染物浓度水平的空间分布与组分特征;研究了多层次深度土壤与地下水污染物之间的相关性。结果表明,园区土壤污染物未超标,但Ni(p=0.018)、Cu(p=0.023)浓度显著高于园区周边,周边的Hg(p=0.074)高于内部;地下水污染物中1,2-二氯乙烷、Mn、Pb、二氯甲烷等多种指标超过国家标准,且部分点位超标程度较高,表明地下水受到了严重污染,同时园区地下水污染物与土壤多层次深度污染物整体相关性较低。本研究为该园区的风险评估和修复方案提供了科学依据,为长江经济带生态环境保护和可持续发展提供了科学支撑。     

华南滨海小流域地下水中PPCPs的分布、来源及影响因素——以珠海市唐家湾镇为例

药物和个人护理用品(Pharmaceutical and Personal Care Products,PPCPs)是在环境中长期存在并对人类乃至整个生态系统的健康造成威胁的两类化学消费品。珠江三角洲流域PPCPs的检出水平总体较高,沿海地区地下水中的PPCPs污染有待进一步探究。于2021年9月在珠海市唐家湾镇采集了16个地下水样本,使用LC-MS/MS分析技术对21种PPCPs进行检测,使用数理统计方法和相关性分析对研究区地下水中PPCPs浓度特征和污染来源进行解析,并结合地下水化学特征及统计分析对其影响因素进行探究,旨在为滨海地区地下水的PPCPs特征分析提供案例依据。研究发现,1)研究区地下水呈弱酸至弱碱性,水化学类型多属于HCO₃-Ca型,沿地下水流方向受人为污染的影响越来越显著。2)研究区地下水中检测到6种PPCPs,平均质量浓度和检出率分别为：磺胺甲恶唑(5.51 ng·L^-1,81%)、磺胺甲基嘧啶(1.18 ng·L^-1,100%)、磺胺二甲基嘧啶(0.168 ng·L^-1,25%...     

修订版《美国有毒物质控制法》改回优先适用规定

<正>2014年4月24日来源:Chemical Watch网站众议院提出的一项改革《有毒物质控制法》的最新版草案法案放松了关于州法律优先适用的规定,并为美国环保署(EPA)对现有化学物质进行评估设定了最后期限。环境与经济小组委员会定于4月29日就修订版草案举行一次听证。在《商业活动中的化学品法》的第一版草案中,美国环保署对一种物质的低优先性指定将优先于对该物     

浑河冲洪积平原土壤及浅层地下水中铅的分布特征

为探讨浑河冲洪积扇土壤及浅层地下水中铅的含量、来源及其分布特征,对研究区50个土壤样品、5个地表水样品和22个浅层地下水样品进行了铅含量分析.结果表明,研究区土壤、地表水和浅层地下水均受到了一定程度的铅污染.表层土壤铅含量较高,在17.72—114.46 mg.kg-1之间,受人为污染影响较大;随土壤深度的增加铅含量呈现逐渐降低的趋势,其迁移规律与铬、砷、铜等重金属密切相关,受土壤性质和有机质含量的影响较大,为研究区土壤和浅层地下水环境风险评价及污染防治提供了科学依据.     

Adsorption distribution impact on preferential transport within horizontal flow constructed wetland (HFCW)

Predicting preferential water flow and solute transport in soils is in the interest of scientists and engineers in the fields of agricultural soil, forest hydrology, soil physics and wastewater treatment by constructed wetland. In artificial wetlands, any preferential pathway induces an insufficient residence time of pollutants in the soil, making an incomplete and unfinished biodegradation process, a wrong evaluation of the hydraulic residence time of the system which would hinder its management in a complete system with several entities of treatment and a non-homogeneous growth of the biofilm in the solid filter mass. This paper is a contribution in tracer experiment data analysis within a horizontal flow constructed wetland built in a storm water basin. A two-dimensional numerical model was used to simulate flow and reactive solute transport. The flow model was successfully calibrated in very dry soil conditions. The adsorption profiles used in the reactive transport modeling are those of five molecules: metolachlor, atrazine, deethylatrazine (DEA), deisopropylatrazine (DIA), and hydroxyatrazine (HA). We show that the adsorption distribution is an internal factor of soil which is responsible to the “preferential” pathway transport in a homogeneous gravel texture. The mean residence time of pollutants within the filter is strongly correlated with the average value of the adsorption coefficient. Moreover, we note a lack of significant impact of the heterogeneity of the medium on the statistical moments of breakthrough curve. It appears that a uni-modal breakthrough curve is not significant to the absence of preferential flow in the medium and at least a two-dimensional display can provide sufficient evidence on the presence or absence of preferential pathways. Finally, using a PLS regression, it is possible to perfectly discriminate the number of peaks of concentration and the asymmetry of the breakthrough curve.     

Preferential leaching of nitrate,chloride and phosphate in an Australian clay soil

This paper investigates leaching of water and nutrients (NO^‐ ₃, Cl^‐, PO^3‐ ₄) from the unsaturated layer in an Australian soil using a multisegment percolation system (MPS). Large undisturbed soil cores were collected from a clay‐based, basaltic plain, agricultural soil at Grassmere, 300 km west of Melbourne, Australia. Significant heterogeneity (or preferential flow) of effluent moisture and solutes was detected (one‐way ANO VA, p < 0.001). Fifty percent of the applied nitrate and chloride leached from the soil core within three days after initial application. Hundred percent of the applied nitrate and chloride leached from the soil core within 8 days after application. These results indicate little incorporation into the soil matrix, and possible denitrification or mineralisation. In contrast, after 18 days, less than 1 % of the total applied phosphates leached from the soil, indicating strong adsorption. Our experiments indicate considerable heterogeneity in water flow patterns and solute leaching on a small spatial scale. Very rapid transport of nitrate and chloride through the soil was evident, in comparison phosphate leaching was negligible. These results have important implications for the management of nutrient schedules in agricultural soils, particularly those located in the Western District of Victoria, Australia.     

蚯蚓活动对重金属在土柱中淋溶行为的影响

采用土柱淋溶方法,以溴离子为示踪离子,研究了蚯蚓活动形成的土壤大孔隙对铜和锌离子在土柱中迁移行为的影响.运用平衡和非平衡对流-弥散模型对溴离子和铜、锌离子在不同土柱中的穿透曲线进行拟合.结果表明,蚯蚓活动形成的蚯蚓孔能够产生明显的优势流现象,这种优势流极大地加快了重金属离子在土柱中垂直向下迁移的速度.非平衡对流-弥散模型能很好地预测溴离子和铜、锌离子在蚯蚓孔土柱中的流出趋势,而平衡对流-弥散模型适合于预测溶质在对照（匀质）土柱中的流出趋势.     

有机污染物在土壤和地下水中迁移建模

地下水有机污染是由人类活动引起的各种物理、化学和生物等干扰过程造成有机污染物自土壤表面迁移至地下含水层的结果。为了解有机污染物如何自土表经过不饱和层（包气带）进入含水层，需要对不饱和层中所进行的各种物理、化学和生物等过程进行较准确的定量描述。本文就不饱和层和含水层中水分和有机污染物迁移建模的一些基本概念和方法进行综述，并列举了一些经典的和新颖的建模方法。     

Quantification of advective solute travel times and mass transport through hydrological catchments

This study has investigated and outlined the possible quantification and mapping of the distributions of advective solute travel times through hydrological catchments. These distributions are essential for understanding how local water flow and solute transport and attenuation processes affect the catchment-scale transport of solute, for instance with regard to biogeochemical cycling, contamination persistence and water quality. The spatial and statistical distributions of advective travel times have been quantified based on reported hydrological flow and mass-transport modeling results for two coastal Swedish catchments. The results show that the combined travel time distributions for the groundwater-stream network continuum in these catchments depend largely on the groundwater system and model representation, in particular regarding the spatial variability of groundwater hydraulic parameters (conductivity, porosity and gradient), and the possible contributions of slower/deeper groundwater flow components. Model assumptions about the spatial variability of groundwater hydraulic properties can thus greatly affect model results of catchment-scale solute spreading. The importance of advective travel time variability for the total mass delivery of naturally attenuated solute (tracer, nutrient, pollutant) from a catchment to its downstream water recipient depends on the product of catchment-average physical travel time and attenuation rate.     

Characteristic volume fractions of different grains in porous media for anomalous dispersion

Anomalous solute transport in porous media is an important issue in groundwater research. In this paper, we explore the relationship between the anomalous solute transport and the volume fractions of different grains in the porous media. Via simulation, we find that there is a maximum and a minimum in the degree of anomalous transport when changing the volume fractions of different grains. Moreover, the characteristic volume fractions corresponding to the anomalous transport maximum and minimum vary little with the flow field and diffusion coefficient of the solute. We also find that the volume fraction corresponding to the most anomalous dispersion is close to the threshold of the site percolation for simple-cubic networks.     

Analytical solution of two-dimensional advection–dispersion equation with spatio-temporal coefficients for point sources in an infinite medium using Green’s function method

In the present study analytical solutions of a two-dimensional advection–dispersion equation (ADE) with spatially and temporally dependent longitudinal and lateral components of the dispersion coefficient and velocity are obtained using Green’s Function Method (GFM). These solutions describe solute transport in infinite horizontal groundwater flow, assimilating the spatio-temporal dependence of transport properties, dependence of dispersion coefficient on velocity, and the particulate heterogeneity of the aquifer. The solution is obtained in the general form of temporal dependence and the source term, from which solutions for instantaneous and continuous point sources are derived. The spatial dependence of groundwater velocity is considered non-homogeneous linear, whereas the dispersion coefficient is considered proportional to the square of spatial dependence of velocity. An asymptotically increasing temporal function is considered to illustrate the proposed solutions. The solutions are validated with the existing solutions derived from the proposed solutions in three special cases. The effect of spatially/temporally dependent heterogeneity on the solute transport is also demonstrated. To use the GFM, the ADE with spatio-temporally dependent coefficients is reduced to a dispersion equation with constant coefficients in terms of new position variables introduced through properly developed coordinate transformation equations. Also, a new time variable is introduced through a known transformation.     

焦化厂多环芳烃污染场地的环境评价实证研究

通过实地调查某焦化厂污染场地污染现状,结果表明：该场地土壤和地下水以多环芳烃（PAHs）有机类污染为主,土壤中苯并（仅）芘和多环芳烃污染以1．5m以内表层土污染为主,随着深度的增加浓度逐渐降低,弱透水层表现出良好的阻隔作用。沿着地下水流动方向,地下水中多环芳烃浓度逐渐降低,经过约400m的迁移,由17296μg／L降至111μg/L;苯并（α）芘经过200m的迁移,由18．3μg／L降至0,地下水流动导致污染物在包气带横向扩散。1号孔、3号孔和4号孔所在地表层土壤中苯并（α）芘的单个污染物的致癌风险分别为0．0278、0．0209和1．496,远远超出可接受水平,因此上述孔位所在地附近表层土壤需重点治理。     

Vegetation competition model for water and light limitation. I: Model description, one-dimensional competition and the influence of groundwater

Vegetation growth models often concentrate on the interaction of vegetation with soil moisture but usually omit the influence of groundwater. However the proximity of groundwater can have a profound effect on vegetation growth, because it strongly influences the spatial and temporal distribution of soil moisture and therefore water and oxygen stress of vegetation. In two papers we describe the behavior of a coupled vegetation-groundwater-soil water model including the competition for water and light. In this first paper we describe the vegetation model, compare the model to measured flux data and show the influence of water and light competition in one dimension. In the second paper we focus on the influence of lateral groundwater flow and spatial patterns along a hillslope. The vegetation model is based on a biophysical representation of the soil-plant-atmosphere continuum. Transpiration and stomatal conductance depend both on atmospheric forcing and soil moisture content. Carbon assimilation depends on environmental conditions, stomatal conductance and biochemical processes. Light competition is driven by tree height and water competition is driven by root water uptake and its water and oxygen stress reaction. The modeled and measured H₂O and CO₂ fluxes compare well to observations on both a diurnal and a yearly timescale. Using an upscaling procedure long simulation runs were performed. These show the importance of light competition in temperate forests: once a tree is established under slightly unfavorable soil moisture conditions it can not be outcompeted by smaller trees with better soil moisture uptake capabilities, both in dry as in wet conditions. Performing the long simulation runs with a background mortality rate reproduces realistic densities of wet and dry adapted tree species along a wet to dry gradient. These simulations show that the influence of groundwater is apparent for a large range of groundwater depths, by both capillary rise and water logging. They also show that species composition and biomass have a larger influence on the water balance in eco-hydrological systems than soil and groundwater alone.     

Biogeochemical transfer and dynamics of iodine in a soil–plant system

Radioactive iodide (¹²⁵I) is used as a tracer to investigate the fate and transport of iodine in soil under various leaching conditions as well as the dynamic transfer in a soil–plant (Chinese cabbage) system. Results show that both soils (the paddy soil and the sandy soil) exhibit strong retention capability, with the paddy soil being slightly stronger. Most iodine is retained by soils, especially in the top 10 cm, and the highest concentration occurs at the top most section of the soil columns. Leaching with 1–2 pore volume water does not change this pattern of vertical distributions. Early breakthrough and long tailing are two features observed in the leaching experiments. Because of the relatively low peak concentration, the early breakthrough is really not an environmental concern of contamination to groundwater. The long tailing implies that the retained iodine is undergoing slow but steady release and the soils can provide a low but stable level of mobile iodine after a short period. The enrichment factors of ¹²⁵I in different plant tissues are ranked as: root > stem > petiole > leaf, and the ¹²⁵I distribution in the young leaves is obviously higher than that in the old ones. The concentrations of ¹²⁵I in soil and Chinese cabbage can be simulated with a dual-chamber model very well. The biogeochemical behaviors of iodine in the soil-cabbage system show that cultivating iodized cabbage is an environmentally friendly and effective technique to eliminate iodine deficiency disorders (IDD). Planting vegetables such as cabbage on the ¹²⁹I-contaminated soil could be a good remediation technique worthy of consideration.