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381.
Davey L. Jones John F. Farrar Kevin K. Newsham 《Water, Air, & Soil Pollution: Focus》2004,4(6):169-175
Amino acids constitute one of the largest inputs of organic nitrogen (N) to most polar soils and have been hypothesized to be important in regulating vegetational succession and productivity in Arctic ecosystems. Our understanding of amino acid cycling in these soils, however, is poor. The aim of this study was to investigate the size and rate of turnover of the amino acid pool in a range of Arctic and Antarctic soils. Our results indicate that in polar soils with either high or low ornithogenic inputs the amino acid pool is small in comparison to the inorganic N pool (NO–3 and NH+4). The free amino acid pool constituted only a small proportion of the total dissolved organic nitrogen (DON) pool in these soils. Here we show that these low concentrations may be due to rapid use by the soil microbial community in both Arctic and Antarctic soils. The turnover of the amino acid pool in soil was extremely rapid, with a half-life ranging from 2 to 24 h, indicating that this N pool can be turned over many hundred times each summer when polar soils are frequently unfrozen. The implications of amino acids in N cycling and plant and microbial nutrition are discussed. 相似文献
382.
Steven N. Chillrud Richard F. Bopp James M. Ross Damon A. Chaky Sidney Hemming Edward L. Shuster H. James Simpson Frank Estabrooks 《Water, Air, & Soil Pollution: Focus》2004,4(2-3):469-482
Radionuclide, radiogenic lead isotope and trace metal analyses on fine-grained sediment cores collected along 160 km of the upper and tidal Hudson River were used to examine temporal trends of contaminant loadings and to develop radiogenic lead isotopes both as a stratigraphic tool and as tracers for resolving decadal particle transport fluxes. Very large inputs of Cd, Sb, Pb, and Cr are evident in the sediment record, potentially from a single manufacturing facility. The total range in radiogenic lead isotope ratios observed in well-dated cores collected about 24 km downstream of the plant is large (e.g., maximum difference in 206Pb/207Pb is 10%), characterized by four major shifts occurring in the 1950s, 1960s, 1970s and 1980s. The upper Hudson signals in Cd and radiogenic lead isotopes were still evident in sediments collected 160 km downstream in the tidal Hudson. The large magnitude and abrupt shifts in radiogenic lead isotope ratios as a function of depth provide sensitive temporal constraints that complement information derived from radionuclide analyses to significantly improve the precision of dating assignments. Application of a simple dilution model to data from paired cores suggests much larger sediment inputs in one section of the river than previously reported, suggesting particle influxes to the Hudson have been underestimated. 相似文献
383.
超声-双氧水和亚铁离子体系处理含酚废水研究 总被引:3,自引:2,他引:3
在实验装置上对超声-双氧水和亚铁离子体系联合处理含酚废水进行了实验研究。主要考察了废水初始pH值、初始双氧水浓度、超声功率、反应时间等因素对酚去除率的影响。实验结果表明:超声辐射可以在双氧水和亚铁离子体系氧化过程中起加速反应的作用,而且随着超声功率的增大,加速反应的能力增强;实验条件下废水初始pH值为4~6.8,初始双氧水浓度为140mg/L时酚去除效果最佳;超声-双氧水和亚铁离子体系处理含酚废水过程中苯酚的降解规律符合表现一级反应。 相似文献
384.
385.
Ton H. Snelder Barry J.F. Biggs Mark A. Weatherhead 《Journal of the American Water Resources Association》2004,40(1):1-13
ABSTRACT: A method is demonstrated for the development of nutrient concentration criteria and large scale assessment of trophic state in environmentally heterogeneous landscapes. The method uses the River Environment Classification (REC) as a spatial framework to partition rivers according to differences in processes that control the accrual and loss of algae biomass. The method is then applied to gravel bed rivers with natural flow regimes that drain hilly watersheds in New Zealand's South Island. An existing model is used to characterize trophic state (in terms of chlorophyll a as a measure of maximum biomass) using nutrient concentration, which controls the rate of biomass accrual, and flood frequency, which controls biomass loss. Variation in flood frequency was partitioned into three classes, and flow data measured at 68 sites was used to show that the classes differ with respect to flood frequency. Variation in nutrient concentration was partitioned at smaller spatial scales by subdivision of higher level classes into seven classes. The median of flood frequency in each of the three higher level classes was used as a control variable in the model to provide spatially explicit nutrient concentration criteria by setting maximum chlorophyll a to reflect a desired trophic state. The median of mean monthly soluble reactive phosphorus and soluble inorganic nitrogen measured at 68 water quality monitoring sites were then used to characterize the trophic state of each of the seven lower level classes. The method models biomass and therefore allows variation in this response variable to provide options for trophic state and the associated nutrient concentrations to achieve these. Thus it is less deterministic than using reference site water quality. The choice from among these options is a sociopolitical decision, which reflects the management objectives rather than purely technical considerations. 相似文献
386.
Gregory F. Mclsaac Matthew B. Short George Groschen Paul Terrio 《Journal of the American Water Resources Association》2004,40(2):443-459
ABSTRACT: Long term data on surface water quality can sometimes be assembled by combining data collected by different agencies at different times and assuming that between agency differences in data quality are insignificant. The objective of this paper was to assess the quality of riverine nitrate (NO3) concentrations in Illinois measured and reported by four agencies from 1967 to 1974 by comparing median values for similar sampling locations and periods. A total of 17 river reaches were identified for which two agencies reported NO3 concentrations during similar periods. Nonparametric comparison of median values and analysis of covariance with discharge as a covariant produced similar results. Nitrate concentrations reported by the U.S. Geological Survey (USGS) from 1967 to 1971 were not statistically (P > 0.05) different from values reported by the Illinois State Water Survey (ISWS) for two of three river reaches. Additionally, NO3 concentrations reported by USGS from 1972 to 1974 were not statistically different than concentrations reported by the Illinois Environmental Protection Agency (IEPA) for four of five river reaches. From 1969 to 1971, NO3 concentrations reported by the Illinois Department of Public Heath and the Illinois Environmental Protection Agency (IDPH/IEPA) were less than one‐fourth the magnitude of values reported by ISWS. The median NO3 concentrations measured by the Central Illinois Public Service (CIPS) were significantly greater than those measured by USGS and IDPH/IEPA in the three comparable sampling locations. The use of NO3 concentrations measured by CIPS and IDPH/IEPA prior to 1972 is not recommended. 相似文献
387.
James F. Saunders Marylee Murphy Martyn Clark William M. Lewis 《Journal of the American Water Resources Association》2004,40(5):1339-1349
ABSTRACT: Historical flow records are used to estimate the regulatory low flows that serve a key function in setting discharge permit limits through the National Pollutant Discharge Elimination System, which provides a nationwide mechanism for protecting water quality. Use of historical records creates an implicit connection between water quality protection and climate variability. The longer the record, the more likely the low flow estimate will be based on a broad set of climate conditions, and thus provides adequate water quality protection in the future. Unfortunately, a long record often is not available at a specific location. This analysis examines the connection between climate variability and the variability of biologically based and hydrologically based low flow estimates at 176 sites from the Hydro‐Climatic Data Network, a collection of stream gages identified by the USGS as relatively free of anthropogenic influences. Results show that a record of 10 to 20 years is necessary for satisfactory estimates of regulatory low flows. Although it is possible to estimate a biologically based low flow from a record of less than 10 years, these estimates are highly uncertain and incorporate a bias that undermines water quality protection. 相似文献
388.
地震灾害对中国农村居民的影响研究--以云南省大姚县为例 总被引:8,自引:0,他引:8
通过对2003年7月21日和10月16日分别发生6.2和6.1级地震的云南省大姚县居民的问卷调查,分析了地震灾害对中困农村居民的影响,了解了我国农村居民尤其是地震多发区农村居民对地震灾害的风险意识以及在地震灾害中的反应.调查结果表明:中国农村居民是地震灾害的最大受害者和风险承担者.虽然他们会在地震灾害中汲取经验教训,增强风险防范意识,但是由于经济水平、自然环境等客观条件的影响,他们只能被动地承受地震灾害,而不能从根本上改变承灾体的脆弱性.中国农村地震减灾、防灾能力的加强需要政府管理部门的积极参与. 相似文献
389.
390.
BaO/γ-Al2O3同时吸附脱除一氧化氮和二氧化硫 总被引:1,自引:0,他引:1
利用固定床连续流动反应器研究了BaO/γ—Al2O,同时吸附模拟烟气中NO和SO2的工艺条件和再生循环使用性能,对BaO/γ—Al2O3进行了比表面积和程序升温表面反应(TPSR)等表征分析。结果表明,BaO/γ—Al2O3的适宜工艺条件是SO2与NO体积比为2.9~8.4、原料气中O2体积分数大于4.5%、吸附温度448~523K。BaO/γ—Al2O3在循环使用过程中吸附能力下降。与NOXSO吸附催化剂Na2CO3/γ—Al2O3相比,BaO/γ-Al2O3同时吸附SO2和NO的能力大、再生循环使用性能好、适宜的SO2与NO体积比范围宽、热稳定性好。将BaO/γ—Al2O3应用于NOXSO工艺可望提高该工艺的脱硫、脱氮效率。 相似文献