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采用高效藻类塘与水生植物塘联用工艺对劣Ⅴ类河水进行深度净化,通过对出水中CODCr,NH4+-N,TP和DO等指标的分析测定,研究了其对沈阳某河流水体的净化效果。结果表明,在HRT为4 d,水深0.5 m,进水CODCr为70~100 mg/L,DO,NH4+-N,TN和TP浓度分别为0.89~1.65,1.6~2.9,2.3~4.5和0.6~1.2 mg/L的条件下,联用工艺出水CODCr为35.40 mg/L,DO,NH4+-N,PO43--P,TN和TP浓度分别为5.88,0.66,0.17,1.51和0.16mg/L,水体中各项指标均达到GB 3838—2002《地表水环境质量标准》中规定的Ⅴ类标准。水生植物塘对藻类塘出水中的藻类有很好的去除效果,平均去除率为94.5%。联用工艺对CODCr,NH4+-N和PO43--P的去除效果均表现为一级藻类塘>二级藻类塘>水生植物塘,其中藻类塘起主要作用。 相似文献
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为探究围垦养殖与退塘还湿对河口湿地土壤铁-碳结合特征的影响,本研究选择福建省闽江河口天然湿地、养殖塘以及退塘还湿样地为研究对象,对3个类型中的土壤铁结合态有机碳(Fe-OC)及其相关指标进行测定与分析.结果显示:①湿地围垦养殖显著影响土壤Fe-OC含量,其含量在退塘还湿后有所回升;②土壤氧化还原过程显著影响土壤中铁相的转化,湿地围垦后土壤中无定形态铁(Feo)与络合态铁(Fep)含量显著下降(p<0.05),而退塘还湿后土壤中游离态铁(Fed)含量显著下降(p<0.05);③养殖塘复湿初期,土壤总有机碳(SOC)含量低于养殖塘,且3样地中土壤Fe-OC均主要以吸附途径结合,其在土壤总有机碳中的占比为4.25%~7.85%;④土壤Fe-OC含量与土壤SOC、Fep、氧化铁的络合度呈显著正相关(p<0.01),与土壤Feo含量呈显著正相关(p<0.05),土壤容重和pH是影响土壤Fe-OC含量的重要环境因素.湿地围垦养殖与退塘还湿能够显著影响土壤Fe-OC含量,相比天然湿地,土壤Fe-OC含量在围垦后持续下降,在复湿过程中有所回升.结果表明退塘还湿对增加湿地碳汇功能具有积极意义. 相似文献
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Benjamin J. Koch Catherine M. Febria Muriel Gevrey Lisa A. Wainger Margaret A. Palmer 《Journal of the American Water Resources Association》2014,50(6):1594-1607
A comprehensive synthesis of data from empirically based published studies and a widely used stormwater best management practice (BMP) database were used to assess the variability in nitrogen (N) removal performance of urban stormwater ponds, wetlands, and swales and to identify factors that may explain this variability. While the data suggest that BMPs were generally effective on average, removal efficiencies of ammonium (NH4), nitrate (NO3), and total nitrogen (TN) were highly variable ranging from negative (i.e., BMPs acting as sources of N) to 100%. For example, removal of NO3 varied from (median ±1 SD) ?15 ± 49% for dry ponds, 32 ± 120% for wet ponds, 58 ± 210% for wetlands, and 37 ± 29% for swales. Across the same BMP types, TN removal was 27 ± 24%, 40 ± 31%, 61 ± 30%, and 50 ± 29%. NH4 removal was 9 ± 36%, 29 ± 72%, 31 ± 24%, and 45 ± 34%. BMP size, age, and location explained some of the variability. For example, small and shallow ponds and wetlands were more effective than larger, deeper ones in removing N. Despite well‐known intra‐annual variation in N fluxes, most measurements have been made over short time periods using concentrations, not flow‐weighted N fluxes. Urban N export is increasing in some areas as large storms become more frequent. Thus, accounting for the full range of BMP performance under such conditions is crucial. A select number of long‐term flux‐based BMP studies that rigorously measure rainfall, hydrology, and site conditions could improve BMP implementation. 相似文献
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AbstractMethane, which is an important greenhouse gas, has received less attention regarding its flux in ponds. Small ponds, whose area only occupies approximately 8.6%, comprise the bulk of CH4 efflux from lakes and ponds on a global scale. However, temporal and spatial variability, as well as consequences of CH4 fluxes from ponds, remains unknown. The aim of this study was to examine using 4 field experiments diel methane (CH4) fluxes from a subtropic eutrophic pond in different seasons. For the eutrophic pond, the mean CH4 efflux for all seasons was 1.772?mg/m2/h, and CH4 emissions in summer were approximately three-fold higher than total of winter, spring, and autumn. Methane diffusive emissions were positively correlated with water temperature, dissolved oxygen (DO) and air temperature but negatively related to pH and to the difference between water temperature and air temperature. The diel diffusive CH4 flux among different seasons varied significantly. The CH4 bubble flux did not differ markedly in winter, spring and autumn, but the quantity in summer was significantly different from all other seasons. Bubble is the main pathway for CH4 emissions. The CH4 ebullition flux accounts for 66, 71, 97 and 98% of the total in winter, spring, summer and autumn, respectively. On an annual scale, the CH4 ebullition flux accounts for 77% of the total fluxes (diffusive?+?ebullitive). Our results show that further investigations need to be carried out to probe temporal variability of CH4 fluxes in ponds located in different climate zones for better understanding of the global carbon budget, which is critical to predict future climate changes. 相似文献
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