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.     

碳二馏分加氢反应装置火灾爆炸危险性评价

运用美国道化学公司的火灾爆炸危险指数评价方法 (第七版 ) ,对碳二馏分加氢反应装置的火灾爆炸危险性进行了定量计算和评价 ,其结果表明 ,该装置的火灾爆炸危险等级为“非常大”。为了降低该装置的危险程度 ,笔者提出了采取有效的安全补偿措施 ,以降低单元的危险程度的新思路。通过分析表明 ,针对部分补偿系数对装置进行安全改进 ,能有效地降低其危险性等级 ,同时可以为避免重大危险源火灾爆炸事故 ,提供切实可行的手段和途径。     

“The Kesterson effect”

Hypothesized to be derived from Cretaceous marine sedimentary rocks, selenium contamination of the Kesterson National Wildlife Refuge is traced through irrigation drainage to the source bedrock of the California Coast Ranges. This biogeochemical pathway of selenium is defined here as the “Kesterson effect.” At the refuge ponds, this effect culminated in 1983 in a 64% rate of deformity and death of embryos and hatchlings of wild aquatic birds. From the previous companion paper on irrigation drainage, the Kesterson effect has been implicated in nine of 11 reconnaissance areas studied in the western United States. Deformities have resulted in at least five of these sites. Climatic, geologic, hydrologic, and soil conditions in these reconnaissance areas are similar to those in the area surrounding Kesterson National Wildlife Refuge in the west-central San Joaquin Valley of California. In California, selenium, as selenate, was ultimately found weathered with sulfur from marine sources in soluble sodium and magnesium sulfate salts, which are concentrated by evaporation on farmland soils. The Se, mobilized by irrigation drainage, is bioaccumulated to toxic levels in refuge wetland ponds that are located mainly in hydrologically closed basins and thus act as concentrating disposal points. The depositional environment of the ponds may be similar to that of the nutrient-rich continental shelf edge and slope in which Cretaceous, Eocene, and Miocene sediments found to be seleniferous in the California Coast Ranges were deposited. Bioaccumulation may be therefore a primary mechanism of selenium enrichment in ancient sediments in addition to that of the formerly suggested Cretaceous volcanic pathway.     

Levels and speciation of heavy metals in soils of industrial Southern Nigeria

A knowledge of the total content of trace metals is not enoughto fully assess the environmental impact of polluted soils. Forthis reason, the determination of metal species in solution isimportant to evaluate their behaviour in the environment andtheir mobilization capacity. Sequential extraction procedure wasused to speciate five heavy metals (Cd, Pb, Cu, Ni and Zn) fromfour contaminated soils of Southern Nigeria into sixoperationally defined geochemical species: water soluble,enchangeable, carbonates, Fe-Mn oxide, organic and residual.Metal recoveries were within ± 10% of the independentlydetermined total Cd, Pb, Cu, Ni and Zn concentrations. The highest amount of Cd (avg. 30%) in the nonresidual fractionswas found in the exchangeable fraction, while Cu and Zn weresignificantly associated with the organic fraction. Thecarbonate fraction contained on average 14, 18.6, 12.6, 13 and11% and the residual fraction contained on average 47, 18, 33,50 and 25% of Cd, Pb, Cu, Ni and Zn respectively. Assuming thatmobility and bioavailability of these metals are related to thesolubility of the geochemical form of the metals, and that theydecrease in the order of extraction sequence, the apparentmobility and potential bioavailability for these five metals inthe soil were: Pb > Zn > Cu > Ni > Cd. The mobility indexes ofcopper and nickel correlated positively and significantly withthe total content of metals, while mobility indexes of cadmiumand zinc correlated negatively and significantly with the totalcontent of metals.     

润滑油精制白土渣处理技术研究

介绍了一种回收白土渣中润滑油的新技术－溶剂抽提技术。通过对润滑油回收量的综合比较，确立了实验所用的抽提溶剂及处理工艺的操作条件。结果表明：用石脑油馏分（60℃－90℃）作抽提溶剂，最佳溶剂与白土渣投量比为1：1，抽提次数为2，温度为室温，搅拌时间为15min且回流液中润滑油质量百分比为5％情况下，润滑油回收率为92％左右，并且可形成稳定的循环模式。     

Pollution characteristics of the recent sediments in the Hangzhou section of the Grand Canal, China

Spatial distribution of heavy metals, arsenic and organic matter in recent sediments in the Hangzhou section of the Grand Canal and their relationships were analyzed. The results showed that the concentrations of heavy metals and organic matters varied widely along the canal, and the average geological accumulation factors decreased in the following orders: organic carbon(2.6), zinc(2.1 ), cadmium(2.0), copper( 1.5), lead(1.1), nitrogen(0.9), mercury (0.8), phosphorus(0.4), arsenic(0.2) and chromium(0). Content of heavy metals and organic carbon in the top 10 cm layer were lower than that of lower layers, except for mercury and organic carbon in the S9 section. Contents of organic carbon in the top 50 cm layer of the mud sediments are significantly higher than those undemeath. In the bottom mud layer, there is a concentration peak of the pollutants. In the mud sediments of the canal, cadmium mainly occurred in the Fe and Mn oxide fraction, copper in the organic fraction, lead in the Fe and Mn oxide fraction, and zinc in the carbonate and the Fe and Mn oxide fraction.     

太原地区公路旁土壤中重金属形态分布和生物有效性研究

采用盆栽试验结合形态分析技术研究了太原地区公路旁污染土壤中Pb,Cd,Cu和Zn的形态分布及其生物有效性。研究结果显示:除Cd外,残渣态是主要形态,可交换态的含量很少;土壤中Cd的碳酸盐结合态、可交换态含量较高,残渣态的含量很少;菜园土重金属的生物可利用性和迁移能力的顺序均是Cd>Cu>Zn>Pb,而高粱土的顺序是Cd>Zn>Cu>Pb,菜园土重金属的生物活性和迁移性较高粱土的大。农作物对Cd,Cu和Zn的累积能力远远大于对Pb的累积能力,且Cd,Cu和Zn向地上部转移的速度也明显比Pb快。研究成果将为评估污染土壤中重金属的危害提供科学依据。     

模拟成藏填埋垃圾有机质稳定化与产气的阶段性

通过人工构建模拟生物气藏的大型模拟生物反应器,研究模拟成藏填埋城市生活垃圾有机质厌氧降解及生物气化规律及其机理。结果表明,自然温度条件下,模拟填埋垃圾有机质降解和生物气化具有明显阶段性,与pH、ORP、温度等指标的阶段性变化存在相关性。产气阶段最佳条件包括:最适温度范围为31.0～36.0℃;最适pH范围为5.47～6.75,pH中性条件下产甲烷速率最高;ORP最适范围为-428～-541 mV,产甲烷高峰期ORP值为-519 mV,低于前人关于甲烷菌最适ORP的界定范围。每千克挥发性固体总生物气和甲烷产量分别为128.5 L和77.7 L,生物气和甲烷最大产气量分别为118.0 L/d和82.0 L/d,甲烷最大浓度为70.4%,产气高峰期与甲烷浓度高峰期同时出现。模拟成藏填埋垃圾有机质的稳定化过程具有明显的可诱导特征,关键因子的优化对有机质的降解及生物气化产生明显促进作用。     

Effects of bulking agent addition on odorous compounds emissions during composting of OFMSW

The effects of rice straw addition level on odorous compounds emissions in a pilot-scale organic fraction of municipal solid waste (OFMSW) composting plant were investigated. The cumulative odorous compounds emissions occurred in a descending order of 40.22, 28.71 and 27.83 mg/dry kg of OFMSW for piles with rice straw addition level at ratio of 1:10, 2:10 and 3:10 (mixing ratio of rice straw to OFMSW on a wet basis), respectively. The mixing ratio of rice straw to OFMSW had a statistically significant effect on the reduction of malodorous sulfur compounds emissions, which had no statistically significant effect on the reduction of VFAs, alcohols, aldehydes, ketones, aromatics and ammonia emissions during composting, respectively. The cumulative emissions of malodorous sulfur compounds from piles with the increasing rice straw addition level were 1.17, 1.08 and 0.88 mg/dry kg of OFMSW, respectively. The optimal mixing ratio of rice straw to OFMSW was 1:5. Using this addition level, the cumulative malodorous sulfur compounds emissions based on the organic matter degradation were the lowest during composting of OFMSW.     

Identification of carbonaceous geosorbents for PAHs by organic petrography in river floodplain soils

Organic petrographic analysis was applied to provide direct information on carbonaceous geosorbents for PAHs in river floodplain soils. The anthropogenic OM group (primarily coal and coal-derived particles) displayed large volume amounts for all the soil samples. Distinct PAH concentrations with similar PAH distribution patterns were determined in grain size and density fractions for each sample. Two-ring PAHs had stronger correlation to organic carbon (OC) than black carbon (BC) contents, while heavier PAHs showed correlation to BC, rather than OC. In this study, we combined grain size and density separation, PAH determinations, TOC and BC measurements, and organic petrographic identification, and concluded that two-ring PAHs in soils were associated to coal particles. Other heavier PAHs could be more controlled by black carbon (BC), which were mostly coal-derived particles from former coal mining and coal industrial activity.