云南兰坪县城滑坡地质特征及其成因分析

2000年9月兰坪县城发生特大型山体滑坡,造成重大经济损失,采取挡墙、抗滑桩等措施后,北部边坡局部基本稳定,南部依见明显新变形,2010~2013年尤甚。基于滑坡现状特征及区域地质环境条件分析,提出了以隐伏断裂(F2)为界将滑坡区重新分块,能够合理反映滑坡的变形破坏特征,并为类似滑坡地质勘察加强针对隐伏断裂的影响分析具有重要的借鉴意义。通过分析滑坡体地质及变形破坏特征,认为滑坡的成因主要受控于滑坡区发育的不利岩性条件及地质结构面,水~岩作用是导致岩体崩解破坏诱发滑坡的主要因素。     

Acid-catalyzed heterogeneous reaction of 3-methyl-2-buten-1-ol with hydrogen peroxide

Acid-catalyzed heterogeneous oxidation with hydrogen peroxide(H2O2) has been suggested to be a potential pathway for secondary organic aerosol(SOA) formation from isoprene and its oxidation products. However, knowledge of the chemical mechanism and kinetics for this process is still incomplete. 3-Methyl-2-buten-1-ol(MBO321), an aliphatic alcohol structurally similar to isoprene, is emitted by pine forests and widely used in the manufacturing industries. Herein the uptake of MBO321 into H2SO4–H2O2mixed solution was investigated using a flow-tube reactor coupled to a mass spectrometer. The reactive uptake coefficients(γ) were acquired for the first time and were found to increase rapidly with increasing acid concentration. Corresponding aqueous-phase reactions were performed to further study the mechanism of this acid-catalyzed reaction. MBO321 could convert to 2-methyl-3-buten-2-ol(MBO232) and yield isoprene in acidic media. Organic hydroperoxides(ROOHs) were found to be generated through the acid-catalyzed route,which could undergo a rearrangement reaction and result in the formation of acetone and acetaldehyde. Organosulfates, which have been proposed to be SOA tracer compounds in the atmosphere, were also produced during the oxidation process. These results suggest that the heterogeneous acid-catalyzed reaction of MBO321 with H2O2 may contribute to SOA mass under certain atmospheric conditions.     

生态文明视域下技术创新、产业升级与污染控制的互作效应研究

随着工业化和城市化进程的加快,环境污染问题已成为生态文明建设亟需解决的重要问题.生态文明是对农业文明和工业文明的超越,代表了更为高级的人类文明形态.生态文明建设是体现经济、社会、环境可持续发展以及人与自然和谐共存的重要战略决策.本文从环境质量改善及污染控制的有效性方面,深入剖析了技术创新、产业升级与污染控制之间的互作效应关系,并探讨了有效的实现方式.研究结果旨在为生态文明建设的有效实施和顺利展开提供借鉴和参考价值.     

SDBS/Na+对红壤胶体悬液稳定性的影响

土壤中普遍存在的有机污染物和无机离子与土壤胶体颗粒的相互作用深刻地影响着土壤中一系列物理、化学和生物学过程.选取红壤胶体作为对象,利用动态光散射技术研究了不同浓度十二烷基苯磺酸钠(SDBS)和Na+作用下红壤胶体颗粒的凝聚过程,并结合体系的pH和Zeta电位分析了SDBS/Na+与土壤胶体颗粒相互作用的机制.结果表明:①相同浓度Na+作用下,随着SDBS浓度的升高,土壤胶体悬液稳定性增强.例如120 mmol·L-1Na+作用下,随着SDBS浓度从0 mmol·L-1升高到10 mmol·L-1,凝聚体有效粒径从702 nm下降至193 nm,总体平均凝聚速率从28.6 nm·min-1减小到3.36 nm·min-1;②相同浓度SDBS作用下,随着Na+浓度的升高,体系Zeta电位绝对值显著降低,凝聚体有效粒径逐渐增大,凝聚速率逐渐加快;③仅SDBS作用下,随着SDBS浓度的升高,体系Zeta电位绝对值从47.6 mV增加到62.2 mV,体系pH从6.17升高到6.76,但均小于土壤胶体悬液本身的pH(6.89).因此,SDBS通过疏水作用和静电作用吸附于土壤胶体颗粒表面,增加了颗粒表面的负电荷数量,降低了作用于胶体颗粒表面的有效Na+浓度(SDBS疏水长链的空间阻碍和高浓度SDBS所形成的胶束结构对Na+的吸附),使得胶体悬液稳定性增强,需要添加更多的Na+才能发生凝聚.     

臭氧-混凝交互作用对混凝效果的影响

采用臭氧-混凝联用(臭氧与混凝剂同时投加)和预臭氧混凝(预臭氧后待水中臭氧浓度为0后再投加混凝剂)两种方式处理水样,分析其氧化、混凝效果和消毒副产物生成势(DBPFP)等的差异,研究臭氧-混凝交互作用对处理效果的影响.结果表明,联用和预臭氧混凝效果之间存在明显差异.联用工艺中臭氧与混凝剂间发生交互作用,导致混凝剂水解形态分布发生改变是影响混凝效果的重要原因.联用处理后水样的浊度高于预臭氧混凝,主要原因之一在于臭氧降低了混凝剂水解形态分布中Alb的含量;Cl-DBPFP低于预臭氧混凝出水,是混凝剂Al Cl3及其某些水解形态对臭氧具有催化氧化的作用,促进了消毒副产物前驱物的氧化降解所致.联用对MCAA和CF生成势的去除效果显著强于预臭氧混凝,其中MCAAFP分别为5.6μg·L-1和16.9μg·L-1,CFFP分别为12.5μg·L-1和24.1μg·L-1.臭氧与混凝剂交互作用显著影响混凝效果及消毒副产物的生成,是臭氧和混凝配合使用安全性研究中需要重点关注的内容.因而,相关科研和实际水处理工艺中必须明确预臭氧及混凝剂投加位点和相对次序.     

Zn2+对铁氧化物吸附苄嘧磺隆的影响

研究2种人工合成的铁氧化物对磺酰脲类除草剂--苄嘧磺隆(bensulfuron-methyl,BSM)的吸附,以及Zn2 对供试样品吸附苄嘧磺隆的影响.实验结果表明,用Langmuir、Freundlich、Temkin等方程对供试样品加入Zn2 后吸附BSM的数据进行了拟合,发现供试样品吸附苄嘧磺隆的等温曲线较好地符合Freundlich方程.加入Zn2 后,铁氧化物吸附苄嘧磺隆的量较未加Zn2 有较大幅度的增加,但在苄嘧磺隆的平衡质量浓度较低(＜4 mg/L)时,氧化物吸附苄嘧磺隆的量不随Zn2 浓度的增加而增加;在苄嘧磺隆的平衡质量浓度较高(＞6 mg/L)时,氧化物吸附苄嘧磺隆的量随Zn2 浓度的增加而增加.这可能是Zn2 和苄嘧磺隆被吸附时存在竞争和协同交互作用的结果.     

Identification of a reactive degradation zone at a landfill leachate plume fringe using high resolution sampling and incubation techniques

Vertical small-scale variation in phenoxy acid herbicide degradation across a landfill leachate plume fringe was studied using laboratory degradation experiments. Sediment cores (subdivided into 5 cm segments) were collected in the aquifer and the sediment and porewater were used for microcosm experiments (50 experiments) and for determination of solid organic carbon, solid-water partitioning coefficients, specific phenoxy acid degraders and porewater chemistry. Results from a multi-level sampler installed next to the cores provided information on the plume position and oxygen concentration in the groundwater. Oxygen concentration was controlled individually in each microcosm to mimic the conditions at their corresponding depths. A highly increased degradation potential existed at the narrow plume fringe (37.7 to 38.6 masl), governed by the presence of phenoxy acids and oxygen. This resulted in the proliferation of a microbial population of specific phenoxy acid degraders, which further enhanced the degradation potential for phenoxy acids at the fringe. The results illustrate the importance of fringe degradation processes in contaminant plumes. Furthermore, they highlight the relevance of using high-resolution sampling techniques as well as controlled microcosm experiments in the assessment of the natural attenuation capacity of contaminant plumes in groundwater.     

STABLE ISOTOPE CHARACTERIZATION OF THE IMPACTS OF ARTIFICIAL GROUND WATER RECHARGE1

ABSTRACT: Stable isotopes of deuterium and oxygen-18 of surface and ground water, together with anion concentrations and hydraulic gradients, were used to interpret mixing and flow in ground water impacted by artificial recharge. The surface water fraction (SWF), the percentage of surface water in the aquifer impacted via recharge, was estimated at different locations and depths using measured deuterium/hydrogen (DIH) ratios during the 1992, 1993, and 1994 recharge seasons. Recharged surface water completely displaced the ground water beneath the recharge basins from the regional water table at 7.60 m to 12.16 m below the land surface. Mixing occurred beneath the recharge structures in the lower portions of the aquifer (>12.16 m). Approximately 12 m down-gradient from the recharge basin, the deeper zone (19.15 m depth) of the primary aquifer was displaced completely by recharged surface water within 193, 45, and 55 days in 1992, 1993, and 1994, respectively. At the end of the third recharge season, recharged surface water represented ～50 percent of the water in the deeper zone of the primary aquifer ～1000 m downgradient from the recharge basin. A classic asymmetrical distribution of recharged surface water resulted from the recharge induced horizontal and vertical hydraulic gradients. The distribution and breakthrough times of recharged surface water obtained with stable isotopes concurred with those of major anions and bromide in a tracer test conducted during the 1995 recharge season. This stable isotope procedure effectively quantified mixing between surface and ground water.     

苏南现代化进程中的遥感土地利用动态监测——以苏、锡、常地区为例

地少人多的广大苏南地区早在６０年代已形成了强大的经济实力,改革开放以来,乡镇企业的迅速崛起带动了地区经济的全面发展。随着苏南经济的迅速发展,土地开发和利用方式也发生了较大变化。人地矛盾、人与空间的不协调日益严重。改善投资环境、合理利用城市土地、促进苏南经济的持续、快速发展,必须更好地实现土地利用的动态监测。为了适应这种新的需求,本文以苏、锡、常地区土地动态变化研究为背景,采用人机交互式解译遥感图像,将多时相遥感信息进行复合,用地理信息系统软件进行分析处理并输出图件。并对苏、锡、常地区的土地利用动态变化特点、各类型变化情况进行了具体分析。实践证明,该方法是行之有效的     

INFLUENCING WATER LEGISLATWE DEVELOPMENT WHAT TO DO AND WHAT TO AVOID1

ABSTRACT: Whomever would affect water policy development must influence the water legislative process. This paper discusses in the context of the Model State Water Allocation Code the following ten ideas about doing that: (1) seek the right timing for enactment; (2) set modest goals; (3) prepare a well-drafted proposal; (4) recognize diversity by offering legislative choices; (5) consider the impacts of adoption; (6) make alliances; (7) respect executive influence; (8) become involved in legislative interaction; (9) be flexible; and (10) persist. Heeding these ideas, although not guaranteeing enactment, is sure to be educational for participants and useful to legislators.