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991.
不同剂量(0, 10, 50,100, 200, 500, 1000nmol/L)的微囊藻毒素-LR作用于肝细胞株BRL-3A 24 h.采用激光扫描共焦显微镜,按荧光光漂白后再恢复技术测定BRL-3A的间隙连接细胞间通讯功能,四唑盐法测定BRL-3A细胞增殖,同时分析胆汁酸运输系统抑制剂利福平对两者的阻滞作用.结果表明,微囊藻毒素-LR可以显著地抑制BRL-3A细胞GJIC功能,并促进BRL-3A细胞增殖,两者均呈剂量效应关系.利福平(30靘ol/L)对微囊藻毒素-LR诱导的BRL-3A细胞GJIC功能下调和增殖有明显的抑制作用.微囊藻毒素-LR可诱导BRL-3A细胞膜泡形成.说明微囊藻毒素-LR肝脏毒性及致癌性可能与抑制肝细胞GJIC功能有关. 相似文献
992.
为了探明酸雨对红壤中硼释放的影响,了解土壤缺硼机制,采用室内模拟酸雨淋溶土柱的方法,研究了酸雨作用下红壤中硼的释放特征.结果表明,酸雨加速了红壤中硼的淋溶损失.酸雨作用下红壤中硼的释放随淋溶量的变化具有初期阶段减小,中期阶段显著增大和后期阶段又减小的阶段性特点.模拟酸雨的pH值越低,硼的释放量越高.酸雨对硼释放的这种促进作用,一般表现为中期阶段的影响要大于初期和后期阶段的影响.淋出液中硼含量的动态变化与pH值的变化成负相关关系.供试土壤不同,硼的释放强度和释放特征存在一定的差异性,硼的释放强度和特点明显受土壤硼的背景值和土壤对酸缓冲能力的影响. 相似文献
993.
采用室内模拟酸雨淋溶土柱的方法,研究了酸雨影响下红壤中钴的释放特征与规律.结果表明,酸雨加速了红壤中钴的淋溶损失.酸雨作用下红壤中钴的释放随淋溶量的变化具有阶段性特点,但不同土壤之间其阶段性特点存在一定的差异.在实验所施的淋溶强度下,供试的4种红壤中有3种表现为前期阶段减小和后期阶段增大的规律性,1种表现为前期阶段减小,中期阶段增大和后期阶段减小的规律性.酸雨对红壤中钴释放的促进作用,在短期内有利于提高红壤钴的可给性,但长期的酸雨淋溶可导致红壤因钴的加速淋失而缺钴. 相似文献
994.
995.
利用2018—2021年安徽省空气质量监测数据分析了PM2.5和O3时空分布特征及其引发的健康风险。结果表明:从时间分布来看,2018—2021年安徽省PM2.5年均值下降25.5%,而O3-8 h年均值则保持持平;PM2.5和O3-8 h月均值具有明显的季节变化特征,PM2.5月均质量浓度和超标天数均在冬季达到最大值,O3-8 h月均值和超标天数则在夏季达到最大值。从空间分布来看,PM2.5、O3-8 h年均值和超标天数均为皖北最高,其次为皖中,最后为皖南。夏季O3是主要的健康风险因子,冬季PM2.5是主要的健康风险因子。当PM2.5超标时,除2021年皖北地区外(PM10是主要的健康风险因子),PM2.5均是主要的健康风险因子;当O3-8 h超标时,O3是主要的健康风险因子。 相似文献
996.
997.
Jason S. Lee Belinda L. Daniels David T. Eberiel Richard E. Farrell 《Journal of Polymers and the Environment》2000,8(2):81-89
Soil retrieval, processing and storage procedures can have a profound effect on soil microorganisms. In particular, changes in soil microbial populations may adversely affect the biological activity of a soil and drastically alter the soil's potential to mineralize added substrates. The effects of cold storage on the biodegradation of a series of test polymers was investigated using two soils—a synthetic soil mix (SM-L8) and a field soil (Bridgehampton silt loam) from Rhode Island (RI-1). Biodegradation tests were conducted using freshly prepared/collected soil and again following storage at 4°C for 3 to 8 months. Prior to each biodegradation test, the soils were incubated at 60% water-holding capacity (WHC) and 25°C to rejuvenate the microbial populations; the soils were incubated for periods of 48 h (freshly collected soil) or 25 days (soils stored at 4°C). Soil microbial populations were assessed by enumerating different segments of the population on agar plates containing different selective media. Mineralization of the test polymers (cellulose, poly-3-hydroxybutyrate, and starch acetate, d.s. 1.5) was monitored using standard respirometric techniques. Our results demonstrated that cold storage had a generally negative effect on the soil microbial populations themselves but that its effect on the capacity of the soil microorganisms to degrade the test polymers varied between soils and polymer type. Whereas cold storage resulted in dramatic shifts in the community structure of the soil microbial populations, substantial restoration of these populations was possible by first conditioning the soils at 60% WHC and ambient temperatures for 25 days. Likewise, although the effects of cold storage on polymer mineralization varied with the test polymer and soil, these effects could be largely offset by including an initial 25-day stabilization period in the test. 相似文献
998.
In situ sequential treatment of a mixed contaminant plume 总被引:1,自引:0,他引:1
Groundwater plumes often contain a mixture of contaminants that cannot easily be remediated in situ using a single technology. The purpose of this research was to evaluate an in situ treatment sequence for the control of a mixed organic plume (chlorinated ethenes and petroleum hydrocarbons) within a Funnel-and-Gate. A shallow plume located in the unconfined aquifer at Alameda Point, CA, was found to contain up to 218,000 μg/l of cis-1,2 dichloroethene (cDCE), 16,000 μg/l of vinyl chloride (VC) and <1000 μg/l of 1,1 dichloroethene (1,1 DCE), trans-1,2 dichloroethene (trans-1,2 DCE) and trichloroethene (TCE). Total benzene, toluene, ethylbenzene and xylenes (BTEX) concentrations were <10,000 μg/l. Contaminated groundwater was funneled into a gate, 3.0 m wide, 4.5 m long and 6.0 m deep (keyed into the underlying aquitard) where treatment occurred. The initial gate segment consisted of granular iron, for the reductive dechlorination of the higher chlorinated ethenes. The second segment, the biosparge zone, promoted aerobic biodegradation of petroleum hydrocarbons and any remaining lesser-chlorinated compounds, stimulated by dissolved oxygen (DO) and carbon dioxide (CO2) additions via an in situ sparge system (CO2 was used to neutralize the high pH produced from reactions in the iron wall). Groundwater was drawn through the gate by pumping two wells located at the sealed, downgradient, end. Over a 4-month period an estimated 1350 g of cDCE flowed into the treatment gate and the iron wall removed 1230 g, or 91% of the mass. The influent mass of VC was 572 g and the iron wall removed 535 g, corresponding to 94% mass removal. The other chlorinated ethenes had significantly lower influent masses (3 to 108 g) and the iron wall removed the majority of the mass resulting in >96% mass removal for any of the compounds. In spite of these high removal percentages, laboratory column tests indicated that at these levels of chlorinated contaminants, surface saturation of the iron grains likely contributed to lower than expected reaction rates. In the biosparge zone, mass removal of cDCE appeared to occur predominantly by biodegradation (65%) with volatilization (35%) being an important secondary process. The dominant removal process for VC was volatilization (70%) although significant biodegradation was also indicated (30%). Laboratory microcosm results confirmed the potential for aerobic biodegradation of cDCE and VC. When average influent field concentrations for cDCE and VC were 220,000 and 46,000 μg/l, respectively, the sequential treatment unit removed 99.6% of the total mass and when the influent concentrations decreased to 26,000 and 19,000 μg/l for cDCE and VC, respectively, >99.9% removal within the treatment gate was attained. BTEX compounds were found to be significantly retarded in the iron treatment zone. Although they did eventually break through the granular iron, and into the gravel transition zone, none of these compounds was detected in the biosparge zone. No noticeable interferences between the anaerobic (reductive) and aerobic parts of the system occurred during testing. The results of this experiment show that in situ treatment sequences are viable, although further work is needed to optimize performance. 相似文献
999.
1000.
Importance of Habitat Quality and Landscape Connectivity for the Persistence of Endangered Natterjack Toads 总被引:1,自引:0,他引:1
Abstract: The natterjack toad (Bufo calamita) is endangered in several parts of its distribution, including Belgium, where it occurs mainly in artificial habitats. We parameterized a general model for natterjack population viability analysis (PVA) and tested its sensitivity to changes in the values of basic parameters. Then we assessed the relative efficiency of various conservation measures in 2 situations: a small isolated population and a system of 4 populations connected by rare dispersal movements. We based the population viability analysis on a stage‐structured model of natterjack population dynamics. We parameterized the model in the RAMAS GIS platform with vital rates obtained from our own field experience and from published studies. Simulated natterjack populations were highly sensitive to habitat quality (particularly pond drying), to dispersal from surrounding local populations, and to a lesser extent to values of fecundity and survival of terrestrial stages. Population trajectories were nearly insensitive to initial abundances, carrying capacities, and the frequency of extreme climatic conditions. The simulations showed that in habitats with highly ephemeral ponds, where premetamorphosis mortality was high, natterjack populations nearly always had a very high extinction risk. We also illustrated how low dispersal rates (<1 dispersing individual/generation) efficiently rescued declining local populations. Such source‐sink dynamics demonstrate that the identification and management of source populations should be a high priority. 相似文献