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141.
水体与土壤中天然有机物与铜的络合作用及其影响因素 总被引:5,自引:1,他引:5
采用络合滴定方法测定了不同反应条件下水体DOC和土壤WSOC与铜的络合参数。比较了土壤WSOC与FA、HA及与水体DOC络合参数的差异。实验结果表明:pH降低,络合稳定常数下降;滴定浓度范围降低,测定络合条件稳定常数升高;离子强度上升,络合稳定常数相应下降。2个样的WSOC络合稳定常数测定结果分别为4.66和4.64,高于水体DOC;络合容量分别为0.079和0.023mmol(Cu)/mg(C),低于DOC。考虑到络合位初始浓度与其他因素的影响,WSOC与FA和HA样品的络合能力相差不大。 相似文献
142.
Decreased carbon and nutrient input to boreal lakes from particulate organic matter following riparian clear-cutting 总被引:2,自引:0,他引:2
The plankton communities of oligotrophic Canadian Shield lakes are strongly regulated by the allochthonous supply of total phosphorus (TP) and dissolved organic carbon (DOC), a proportion of both of which originate from particulate organic matter. Although decreased inputs of allochthonous leaf litter have been documented for small streams whose riparian forests have been removed, no such data exist for boreal lakes. Through estimates of airborne litter input from forested and clear-cut shorelines and laboratory measurements of concentrations released from leaf leachate, we determined that riparian deforestation resulted in reductions of DOC from 17.8 to 0.4 g/m shoreline/yr and of TP from 2.9 to 0.3 g/m shoreline/yr. Previous predictive models indicate that such reductions may be substantial enough to decrease basic metabolic processes of lake plankton communities by as much as 9% in primary production and 17% in respiration. 相似文献
143.
Impact of Lime and Ash Applications on Soil Solution Chemistry of an Acidified Podzolic Soil 总被引:2,自引:0,他引:2
Geibe Christine E. Holmström Sara J. M. Van Hees Patrick A. W. Lundström Ulla S. 《Water, Air, & Soil Pollution: Focus》2003,3(4):77-96
Soil solution samples were taken from two sites (Horröd and Hasslöv) in the south part of Sweden to evaluate how soil solution chemistry responded to different treatmentswith dolomite and wood ash. At Horröd, samples were taken four years after application of wood ash, 4.28 ton ha-1 and dolomite, 3.25 ton ha-1. At Hasslöv dolomite, 3.45 ton ha-1 and 8.75 ton ha-1 was applied and samples were taken 15 yr later. It was found that treatment with dolomite at one site (Hasslöv) resulted in higher pH values (<2 pH units) and higher nitrification. It was also found at this site that the total Al and the inorganic Al concentrations decreased with dolomite treatment. The Ca, Mg, DOC, Fe, SO4
2- and Cl- concentrations, mainly in the topsoil, were found to be higher at both sites, following dolomite treatment; Ca and Mg concentrations were 2–8 times higher (<820 M) than in controls (<70 M). Wood ash was found to have less impact. The PO4 concentration in the O2 horizon at Hasslöv decreased due to dolomite-treatment. ANOVA (Analyse of Variance) and PLS (Partial Least Square) were used to evaluate the data from the two sites. 相似文献
144.
Nelson J. ODriscoll Emma Vost Erin Mann Sara Klapstein Robert Tordon Matthew Lukeman 《环境科学学报(英文版)》2018,30(6):151-159
Mercury is a globally distributed, environmental contaminant. Quantifying the retention and loss of mercury is integral for predicting mercury-sensitive ecosystems. There is little information on how dissolved organic carbon(DOC) concentrations and particulates affect mercury photoreaction kinetics in freshwater lakes. To address this knowledge gap,samples were collected from ten lakes in Kejimkujik National Park, Nova Scotia(DOC: 2.6–15.4 mg/L). Filtered(0.2 μm) and unfiltered samples were analysed for gross photoreduction, gross photooxidation, and net reduction rates of mercury using pseudo first-order curves. Unfiltered samples had higher concentrations(p = 0.04) of photoreducible divalent mercury(Hg(II)RED)(mean of 754 ± 253 pg/L) than filtered samples(mean of 482 ± 206 pg/L);however, gross photoreduction and photooxidation rate constants were not significantly different in filtered or unfiltered samples in early summer. DOC was not significantly related to gross photoreduction rate constants in filtered(R~2= 0.43; p = 0.08) and unfiltered(R~2= 0.02; p = 0.71) samples; DOC was also not significantly related to gross photooxidation rate constants in filtered or unfiltered samples. However, DOC was significantly negatively related with Hg(Ⅱ)_(RED) in unfiltered(R2= 0.53; p = 0.04), but not in filtered samples(R~2= 0.04;p = 0.60). These trends indicate that DOC is a factor in determining dissolved mercury photoreduction rates and particles partially control available Hg(Ⅱ)_(RED) in lake water. This research also demonstrates that within these lakes gross photoreduction and photooxidation processes are close to being in balance. Changes to catchment inputs of particulate matter and DOC may alter mercury retention in these lakes and could partially explain observed increases of mercury accumulation in biota. 相似文献
145.
在一台原机为满足国Ⅲ排放法规的增压中冷电控单体泵四缸发动机上采用柴油/甲醇双燃料(DMDF)燃烧方式,结合废气再循环(EGR)技术及不同后处理装置进行台架试验.结果表明:加装DMDF系统并经过精细标定,在不添加任何后处理器的情况下,仅结合EGR,氮氧化物(NOx)和颗粒物(PM)的排放即可满足国V规定法规,但总碳氢化合物(THC)和一氧化碳(CO)排放高于法规限值;增加采用氧化催化转化器(DOC)或DOC+颗粒氧化催化转化器(POC)简单的后处理装置可以使电控单体泵DMDF发动机排放全面满足国V排放标准要求.其中,仅采用DOC的方式,THC和CO十三点加权比排放与后处理之前相比的降幅可分别达98.0%和99.8%,且分别仅为国V限值的35.2%和2.4%,采用DOC+POC的方式,HC和CO十三点比排放较原机的降幅分别达99.2%和99.9%,且分别仅为国V限值的13.5%和1.2%. 相似文献
146.
太湖梅梁湾有色可溶性有机物对光的吸收 总被引:24,自引:2,他引:24
探讨了太湖梅梁湾不同湖区有色可溶性有机物(CDOM)对光的吸收、光衰减系数的变化及与DOC浓度的关系、CDOM吸收对光衰减系数的贡献率以及指数函数曲线斜率S值.结果表明,不同类型湖区CDOM吸收系数差异明显,ad(440)、ad(320)的变化范围分别为1.22~2.58m-1,6.24~10.69m-1;DOC浓度最高值出现在梁溪河口,为12.74mg/L,最低值出现梅梁湾口,为6.87mg/L,大致呈由湾内向湾口逐渐递减的趋势;DOC与CDOM吸收系数在波长320nm以下存在显著性相关,波长320~700nm CDOM吸收对光衰减系数的贡献率在0.69%~60.9%间变化,400nm以下紫外短光部分贡献率均大于20%,空间上短波部分贡献率在河口区、五里湖比梅梁湾内及沿岸带要大;CDOM吸收的指数函数曲线斜率S在13.9~18.1m-1间. 相似文献
147.
正Introduction Natural organic matter(NOM)present in source water has significant impact on water treatment processes and on the quality of drinking water.NOM is a complex mixture of diverse groups of organic compounds,humic and fulvic acids,proteins,peptides,carbohydrates,and heterogeneous materials 相似文献
148.
湿地垦殖对土壤微生物量及土壤溶解有机碳、氮的影响 总被引:8,自引:4,他引:8
对三江平原天然沼泽湿地及湿地垦殖后的农田、弃耕还湿地、人工林地等不同土地利用方式下表层土壤(0~10cm)的活性碳、氮组分:微生物量碳(MBC)、微生物量氮(MBN)、溶解有机碳(DOC)、溶解有机氮(DON)进行了研究.结果表明,天然小叶章沼泽湿地垦殖为农田后,表层土壤各活性碳、氮组分显著降低:MBC减少了63.8%~80.5%; MBN减少了56.3%~67.1%; DOC减少了43.1%~44.3%; DON减少了25.2%~56.1%.农田弃耕还湿和人工造林后表层土壤的活性碳、氮组分有明显恢复的趋势,各组分恢复到天然小叶章湿地土壤水平的36.1%~59.9%(MBC);46.7%~65.9%(MBN);67.0%~69.3%(DOC);81.2%~88.3%(DON),土地利用方式是影响土壤MBC、MBN、DOC、DON变化的重要因素;各土地利用方式表层土壤的DOC、DON、MBC、MBN呈显著的正相关关系,土地利用方式对表层土壤DOC的影响大于对DON的影响;各土地利用方式下土壤微生物可利用碳、氮的来源不同是影响DOC、DON与MBC、MBN相关性差别明显的主要原因. 相似文献
149.
选用某污水处理厂的二沉池出水[(TN主要以硝态氮(NO3--N)形式存在)作为研究对象,采取水培植物生态槽进行脱氮试验,着重研究了NO3--N的反硝化过程.结果表明, NO3--N与COD均得到有效去除;生态槽厌氧区水力停留时间(HRT)为10~18h,系统水力负荷为1.33m3/(m3×d),不投外加碳源时,空槽运行NO3--N去除率为10.80%;种植能分泌溶解性有机碳(DOC)的凤眼莲使NO3--N去除率升至15.89%;而硫自养反硝化过程使NO3--N去除率提高至37.80%;投加葡萄糖时,TN与NO3--N的去除率分别达到87.20%和93.21%,出水浓度分别降到2.2,1.04mg/L. 相似文献
150.