SBR工艺处理维生素C废水试验研究

采用颗粒污泥和普通絮体污泥SBR反应器对维生素C生产废水进行可生化性对比试验研究，结果表明，在进水CODcr为400—1800mg／L，运行周期为8h，其中曝气时间为5．5h，换水比为80％的条件下，颗粒污泥反应器CODer去除率为75-90％，污泥浓度介于6．11～8．32g／L，污泥指数为20～40mL／g.     

污水生物处理过程中的同步硝化反硝化研究概况

在好氧生物氧化过程中通过控制反应器内 DO浓度、C/N比、污泥负荷的条件下 ,观察到较明显的同步硝化反硝化现象 ,通过控制反应条件 ,可使硝化、反硝化速率都得以同步提高。     

单片机串口通信平台的搭建

文章介绍了串口通信的基本概念、基本原理、RS-232C标准、地震数据采集器与MCS-51单片机的通信连接，同时介绍了串口通信在地震数据传输中的实际应用。     

New process for anaerobic treatment of Vitamin C wastewater in a full scale plant

１ＩｎｔｒｏｄｕｃｔｉｏｎＴｈｅＦｉｒｓｔＰｈａｒｍａｃｅｕｔｉｃａｌＦａｃｔｏｒｙｉｎＳｈｉｊｉａｚｈｕａｎｇＣｉｔｙ，Ｃｈｉｎａ，ｂｕｉｌｔａｓｅｔｏｆｅｑｕｉｐｍｅｎｔｏｆｆｕｌｓｃａｌｅｔｒｅａｔｉｎｇＶｉｔａｍｉｎＣｗａｓｔｅｗａｔｅｒｉｎ...     

Technical and theoretical considerations in the HLA typing of amniotic fluid cells for prenatal diagnosis and paternity testing

HLA typing of amniotic fluid cells has been used for the prenatal diagnosis of the HLA linked diseases congenital adrenal hyperplasia (21-OH-deficiency (21-OH-def) type) and complement C4 deficiency and it has also been used for the prenatal de termination of paternity. There are, however, technical difficulties in this test associated with the weak expression of some B locus antigens on amniotic fluid cells, and theoretical difficulties related to associations between particular HLA antigens and the 21-OH-def allele. Since certain HLA-B locus antigens are found in significantly increased frequencies among patients with 21-OH-def, there is a relatively high incidence of HLA-B homozygosity among the patients and over 40 percent of the parents of these patients share one or more HLA-B locus antigens. Results of some prenatal HLA typing tests may thus be difficult to interpret, and supplementary tests should be used whenever possible. HLA typing of amniotic cells is, however, the only available procedure for prenatal diagnosis of C4 deficiency and it is the best available procedure for prenatal determination of paternity. A modification of our original procedure allows HLA typing to be performed with increased numbers of HLA typing sera, and sera with optimum reactivity for amniotic fluid cells have now been selected for the definition of most of the more commonly expressed HLA antigens. Although amniotic fluid cells do not express DR antigens, amniotic fluid cells can be typed for the HLA-linked marker glyoxalase I (GLO) and this may be the informative for prenatal diagnosis in some cases.     

First-trimester prenatal diagnosis of Sanfilippo C disease

At 10 weeks' gestation, chorionic villus biopsy was obtained from a woman at risk for Sanfilippo type C disease. Acetyl-CoA: α-glucosaminide N-acetyltransferase activity was markedly deficient. The pregnancy was terminated at 12 weeks' gestation and follow-up study on fetal fibroblasts confirmed the diagnosis.     

沼泽湿地孔隙水中溶解有机碳、氮浓度季节动态及与甲烷排放的关系

选择三江平原典型的毛果苔草沼泽湿地为研究对象,测定了沼泽湿地孔隙水中水溶性碳、氮浓度、CH4浓度和CH4排放通量,以及相关环境因子;研究了沼泽水中水溶性有机碳、氮浓度变化特征,探讨了沼泽湿地孔隙水中CH4浓度和排放通量季节性变化及发生原因.结果表明,三江平原沼泽湿地土壤孔隙水中DOC浓度有明显的季节变化(p＜0.01).最高值(剖面平均值为95.1 mg·L-1)出现在6月份,9和10月份出现最低值(剖面平均值均为79.3 mg·L-1),剖面上浓集中心位于15～30 cm.孔隙水中NH4 -N和NO-3-N浓度也有明显的季节变化,而DON变化不明显.孔隙水中CH4浓度在剖面上的分布特征与DOC一致,高浓度中心位于20～30 cm.除6月份外,孔隙水甲烷浓度与土壤温度和DOC浓度有显著的正相关关系,与NH4 -N和NO3-N均没有显著相关性.土壤温度和孔隙水中DOC浓度是影响沼泽湿地产CH4能力的重要因素.CH4排放通量与土壤温度和积水深度呈很好的指数关系,与剖面CH4浓度和孔隙水NH4 -N浓度有显著的正相关关系.CH4排放通量与孔隙水DOC浓度相关性不显著.     

应用δ~(13)C值探讨土壤中有机碳的迁移规律

C3 植物与C4 植物具明显的δ13C值差异 ,利用这种特性 ,选取荔波茂兰喀斯特森林边缘处这个C3植物—C4 植物转换生长的地点 ,分别采集森林与农田各三个剖面的土壤样品 ,根据测定其土壤总有机碳、不同粒径及不同比重组分的δ13C值间的相互关系来推导土壤有机碳的若干迁移规律     

Carbon isotope ratios in logged and unlogged boreal forests: Examination of the potential for determining wildlife habitat use

Due to assimilation of recycled CO₂ from litter decomposition and photosynthetic changes in carbon fractionation at low light levels, the foliage at the base of a forest is often more depleted in¹³C compared to that exposed to the atmosphere in either the canopy or in open clearings. This is referred to as the canopy effect. African research has indicated that these habitat differences in foliar ¹³C can be substantial enough to affect the carbon isotope ratios of resident fauna. Previous work documenting a 30-year chronology on moose teeth from Isle Royale National Park indicated a progressive depletion in¹³C and suggested that this could be due to forest regrowth following extensive burning. The present study examined the assumption implicit in this hypothesis that foliar ¹³C varies between open and closed boreal forest sites. I found a marginal canopy effect of 2 ¹³C difference between upper canopy and ground flora for a forest in northwestern Ontario and an average difference of 1.2 in under- and mid-story vegetation between closed forests and open clear-cuts. Because of these small differences, the utility of carbon isotope analysis in quantifying temporally integrated exploitation of deforested habitats will be low for northern boreal locations. In denser forests, such as those in the tropics or western North American where the canopy effect can be expected to be much greater, ¹³C analysis may still offer some promise for determining selection by wildlife of disturbed habitats.     

Characterisation of Organic Matter and Carbon Cycling in Rehabilitated Lignite-rich Mine Soils

Open-cast lignite mining in the Lusatian mining district resulted in rehabilitated mine soils containing up to four organic matter types: (1) recent plant litter, (2) lignite deposited by mining activity, (3) carbonaceous ash particles deposited during amelioration of the lignite-containing parent substrate and (4) airborne carbonaceous particles deposited during contamination. The influence of lignite-derived carbon types on the organic matter development and their role in the soil carbon cycle was unknown. This paper presents the findings obtained during a six year project concerning the impact of lignite on soil organic matter composition and the biogeochemical functioning of the ecosystem. The organic matter development after rehabilitation was followed in a chronosequence of rehabilitated mine soils afforested in 1966, 1981 and 1987. A differentiation of the organic matter types and an evaluation of their role within the ecosystem was achieved by the use of ¹⁴C activity measurements, ¹³C CPMAS NMR spectroscopy and wet chemical analysis of plant litter compounds. The results showed that the amount and degree of decomposition of the recent organic matter derived from plant material of the 30 year old mine soil was similar to natural uncontaminated forest soil which suggests complete rehabilitation of the ecosystem. The decomposition and humification processes were not influenced by the presence of lignite. On the other hand it was shown that lignite, which was thought to be recalcitrant because of its chemical structure, was part of the carbon cycle in these soils. This demonstrates the need to elucidate further the stabilisation mechanisms of organic matter in soils.