平朔安太堡矿区复垦地土壤微生物与土壤性质关系的研究

调查安太堡大型露天矿区西排土场植被恢复与土壤微生物的关系.结果表明,土壤中微生物量与土壤中的水分、速效磷、土壤有机质、有效性氮和海拔高度有明显的关系.麦地、林地、草地的土壤中呈现出:细菌》放线菌》固氮菌》霉菌;撂荒地呈现为:细菌》放线菌》霉菌》固氮菌;裸地呈现出:细菌》放线菌》霉菌.细菌、放线菌和霉菌呈现麦地最高,裸地最低,固氮菌为林地高于其他样地.在撂荒地和裸地中,细菌占微生物总量的一半以上.麦地、林地、草地、撂荒地中的各种菌、速效磷、土壤有机质、有效性氮含量明显高于裸地中的含量.微生物总量和样地的海拔、样地土壤的含水率有明显的关系,土壤中的含水量直接影响微生物总量.微生物总量与速效磷含量和有机质含量成正比,有机质含量与有效性氮含量成正比.细菌与海拔呈极显著负相关,与其他几种养分指标呈极显著正相关,放线菌与海拔和速效磷呈极显著相关,与其他指标相关性不显著,固氮菌与几种养分指标相关性均不显著.按全国土壤养分划分标准,安太堡大型露天矿区复垦地等级不高,还需要用科学的方法加快复垦区土壤的恢复.     

臭氧生物活性炭有机物吸附与生物降解量化分析

以西安北石桥污水净化中心出水为研究对象,通过对臭氧-生物陶粒与臭氧-生物活性炭处理工艺的对比研究,分析比较了两种生物过滤系统的生物活性及有机物去除特性,建立了臭氧-生物活性炭工艺在有机物降解过程中吸附和生物降解作用的量化计算方法,探讨了臭氧-生物活性炭工艺有机物降解过程及去除机理.研究表明:臭氧-生物活性炭工艺对有机物的去除是活性炭吸附和生物降解的协同作用,其中生物降解占主导作用,约占有机物总去除量的65%,生物降解作用去除的有机物几乎全部是易于降解的溶解性有机物;而吸附作用去除的有机物约占有机物总去除量的35%,去除的有机物中难降解和易于降解的有机物的量基本相当.     

脉冲电晕放电与CuO/γ-Al2O3协同处理烟气中SO2和NO的实验研究

研究了催化剂CuO/γ-Al2O3与脉冲电晕放电协同作用脱除烟气中的SO2和NO.结果表明, 在100 ℃以下,CuO/γ-Al2O3与脉冲电晕放电协同作用具有较好的脱硫脱氮效果.当脉冲电压40 kV,进口烟气温度80 ℃,出口烟气温度40℃,气体在烟道中的流速为1.3 m/s,SO2的初始质量浓度为1 400 mg/m3,NO的初始质量浓度350 mg/m3,SO2的脱除率达到85%,NO的脱除率达到30%.     

胶州湾沉积物氮的环境生物地球化学意义

利用氮的分级浸取技术,研究了胶州湾不同粒级沉积物中氮的赋存形态.研究表明,胶州湾沉积物中可转化态氮可分为离子交换态、弱酸浸取态、强碱浸取态和强氧化剂浸取态.不同粒级沉积物中各形态氮占可转化态氮的比例各不相同.在细、中和粗粒级沉积物中,强氧化剂浸取态氮是可交换态氮的优势形态,分别占可转化氮的35.38%、44.38%和58.69%.在中、粗粒级沉积物中,强碱浸取态氮是无机氮的主要赋存形态,分别占可转化态氮的26.31%和25.85%.在细粒级沉积物中,离子交换态氮是优势态的无机氮,占可转化态氮的27.67%.相关分析表明,对于胶州湾来说,沉积物的粒度越细,氮的含量就越高,各形态氮大致与细、中粒级沉积物含量呈正相关,而与粗粒级沉积物含量呈负相关.研究还表明,不同粒级沉积物中氮与浮游植物数量、叶绿素a以及上覆水体中硝酸盐的含量大致都在一定程度上呈正相关,这一方面说明了沉积物对上覆水体元素的含量有着不可忽视的影响,另一方面也说明了沉积物中的氮对海水的富营养化水平有着较好的指示和十分重要的环境意义.     

三阶段温度控制堆肥接种法对有机氮变化规律的影响

利用原生生活垃圾,通过三阶段温度控制技术进行堆肥试验,探讨在堆肥过程中有机态氮组分的动态变化规律.结果表明,全氮、酸水解有机态氮、氨基酸态氮均在堆肥的前期呈明显的下降趋势,呈较好的相关性.与CK（对照组）处理相比,在堆肥的后期,三阶段温度控制堆肥酸水解有机态氮、氨基酸态氮、氨基糖态氮及酸解未知态氮含量呈不同程度的上升趋势,增加幅度依次为：10.67%、16.17%、7.17%、22.44%.表明三阶段温度控制技术能减少堆肥中氮素的损失,堆肥产品施入土壤后,可提高土壤的供氮潜力.     

膜生物反应器中进水组成对膜污染的影响

研究了膜生物反应器中进水组成对膜污染的影响. 结果表明, 相对于正常组成来说进水中限氮或限磷引起的膜污染程度更重, 尤以进水中限氮时更为严重. 系统缺氮或缺磷时, 污泥絮体的相对憎水性和膜的憎水性增加, 使得膜和污泥之间的憎水相互作用增强, 加速了污染物在膜表面的沉积和/或吸附. 另外, 进水中限氮或限磷时, 污泥中丝状菌的数量增加, 把颗粒污泥捆扎、束缚在其立体网状结构中, 滤层结构更加致密, 孔隙度减小, 增加了膜污染阻力; 丝状菌的作用还在于它们能够将污染物牢牢地缠绕、固定在膜表面, 加强了膜表面污染物抵御曝气的水力冲刷作用的能力, 从而也加速了膜污染.     

利用嗜酸性硫杆菌的生物产酸作用处理洗毛废水

利用洗毛废水在低pH条件下,有机物絮凝沉降的特点,通过嗜酸性硫杆菌(Acidophilic thiobacillus)的产酸作用降低体系pH,破坏废水固有的稳定性,改变有机物的亲水性能,实现固液分离,达到去除COD的目的.试验结果表明,生物产酸作用能有效地去除废水COD,改善其脱水性能.当体系pH降至3.00, COD去除率达到最大值91.4%,处理后的废水有很好的机械脱水和沉降性能,比阻从大于9.81×10¹³　m·kg^-1降至5.60×10¹¹ m·kg^-1.而对照处理在整个培养期内,未发生明显的改变,仅有20%的COD被去除.本研究为油脂含量高、难被生物利用的有机废水提供了一条新的处理方法.     

Denitrification potential enhancement by addition of external carbon sources in a pre-denitrification process

The aim of this study is to investigate the denitrification potential enhancement by addition of external carbon sources and to estimate the denitrification potential for the predenitrification system using nitrate utilization rate （NUR） batch tests. It is shown that the denitrification potential can be substantially increased with the addition of three external carbon sources, i.e. methanol, ethanol, and acetate, and the denitrification rates of ethanol, acetate, and methanol reached up to 9.6, 12, and 3.2 mgN/（g VSS.h）, respectively, while that of starch wastewater was only 0.74 mgN/（g VSS,h）. By comparison, ethanol was found to be the best external carbon source. NUR batch tests with starch wastewater and waste ethanol were carried out. The denitfification potential increased from 5.6 to 16.5 mg NO3-N/L owing to waste ethanol addition. By means of NUR tests, the wastewater characteristics and kinetic parameters can be estimated, which are used to determine the denitrification potential of wastewater, to calculate the denitrification potential of the plant and to predict the nitrate effluent quality, as well as provide information for developing carbon dosage control strategy.     

Biological control experiment of excess propagation of Cyclops for drinking water security

Cyclops of zooplankton propagated excessively in eutrophic water body and could not be effectively inactivated by the conventional disinfections process like chlorination due to its stronger resistance to oxidation. In this study, an ecological project was put forward for the excess propagation control of Cyclops by stocking the filter-feeding fishes such as silver carp and bighead carp under the condition of no extraneous nutrient feeding. The results of experiments with different stocking biomass showed that the propagation of Cyclops could be controlled effectively, and the water quality was improved simultaneously by impacting on nutriment level and plankton community structure at proper stocking density of 30 g/m^3 of water. The growth of Cyclops may not be effectually controlled with lower biomass of fish （10 g）, and the natural food chain relation may be destroyed for Cyclops dying out in water while the intense stocking of 120 g per cubic meter of water. In addition, the high predator pressure may accelerate supplemental rate of nutrients from bottom sediments to water body to add the content of total nitrogen and phosphorus in water.     

Effects of long-term amendment of organic manure and nitrogen fertilizer on nitrous oxide emission in a sandy loam soil

To understand the effects of long-term amendment of organic manure and N fertilizer on N2O emission in the North China Plain, a laboratory incubation at different temperatures and soil moistures were carried out using soils treated with organic manure （OM）, half organic manure plus half fertilizer N （HOM）, fertilizer NPK （NPK）, fertilizer NP （NP）, fertilizer NK （NK）, fertilizer PK （NK） and control （CK） since 1989. Cumulative N2O emission in OM soil during the 17 d incubation period was slightly higher than in NPK soil under optimum nitrification conditions （25℃ and 60% water-filled pore space, WFPS）, but more than twice under the optimum denitrification conditions （35℃ and 90% WFPS）. N2O produced by denitrification was 2.1-2.3 times greater than that by nitrification in OM and HOM soils, but only 1.5 times greater in NPK and NP soils. These results implied that the long-term amendment of organic manure could significantly increase the N2O emission via denitrification in OM soil as compared to NPK soil. This is quite different from field measurement between OM soil and NPK soil. Substantial inhibition of the formation of anaerobic environment for denitrification in field might result in no marked difference in N2O emission between OM and NPK soils. This is due in part to more rapid oxygen diffusion in coarse textured soils than consumption by aerobic microbes until WFPS was 75% and to low easily decomposed organic C of organic manure. This finding suggested that addition of organic manure in the tested sandy loam might be a good management option since it seldom caused a burst of N2O emission but sequestered atmospheric C and maintained efficiently applied N in soil.