2000—2015年深圳市建设用地坡谱演变研究

在受地形约束的快速城市化地区,建设用地水平扩张常伴有垂直爬坡过程。通过分析建设用地坡谱曲线形态及其变化特征,有助于认识该过程的时空分异及演变规律,进而科学指导相关国土规划实践。论文以深圳市及其所辖10个区为例,利用DEM及2000—2015年遥感影像构建地面坡谱和4期建设用地坡谱,借助陡峭度、均匀度、累加关键值等坡谱研究手段,分析该市建设用地坡谱演变特征。结果表明：深圳市建设用地坡谱变化特征总体表现为爬坡与填海共存,且以爬坡为主,总体爬坡速度保持相对稳定;该市各辖区建设用地坡谱曲线呈现不同变化特征,可归纳为爬坡主导型、填海主导型、混合型和稳定型;各辖区建设用地布局均集中于平缓区域,建设用地上坡程度整体属于轻度至中度,建设用地主流上限坡度分布范围为4°~14°,建设用地极端上限坡度分布范围为7°~20°。深圳市仍将面临建设用地继续爬坡的压力,相关坡度上限标准的科学制定与严格执行是把控建设用地爬坡进程的关键。     

印染废水处理的磁混凝-高梯度磁分离协同作用

混凝过程作为工业废水的预处理技术普遍受到重视,在混凝过程中降低污泥产生量并提高污泥分离速度是该技术发展的方向,基于上述目标,通过将磁粉引入絮体使之磁化并在自行研制的高梯度磁分离装置中实现磁混凝与磁分离的协同作用.以高浊度的印染废水作为试验废水,以色度、COD及SS作为考核指标,重点考察了磁混凝反应及磁分离的影响因素.当印染废水的色度约为900倍、COD约为595 mg/L、SS约为500 mg/L时,在pH=8.5、FeSO4500 mg/L、PAM3.5 mg/L、磁粉400 mg/L的适宜磁混凝反应条件下,相应指标去除率比传统混凝法分别高出17.3%、21.7%及24.2%,此时絮团沉降速度增大了64.3%,污泥体积减少了61%,污泥压缩比为0.39.在电流强度8 A、流速2.5 L/min和介质填充率1%的操作条件下,该磁性絮体流经高梯度磁分离装置时的水力表面负荷达到61.0 m3/m2·h,处理出水达到国家二级排放标准.     

Response of anaerobes to methyl fluoride, 2-bromoethanesulfonate and hydrogen during acetate degradation

To use the selective inhibition method for quantitative analysis of acetate metabolism in methanogenic systems,the responses of microbial communities and metabolic activities,which were involved in anaerobic degradation of acetate,to the addition of methyl fluoride(CH3F),2-bromoethanesulfonate(BES)and hydrogen were investigated in a thermophilic batch experiment.Both the methanogenic inhibitors,i.e.,CH3F and BES,showed their effectiveness on inhibiting CH4 production,whereas acetate metabolism other than acetoclastic methanogenesis was stimulated by BES,as reflected by the fluctuated acetate concentration.Syntrophic acetate oxidation was thermodynamically blocked by hydrogen(H2),while H2-utilizing reactions as hydrogenotrophic methanogenesis and homoacetogenesis were correspondingly promoted.Results of PCR-DGGE fingerprinting showed that,CH3F did not influence the microbial populations significantly.However,the BES and hydrogen notably altered the bacterial community structures and increased the diversity.BES gradually changed the methanogenic community structure by affecting the existence of different populations to different levels,whilst H2 greatly changed the abundance of different methanogenic populations,and induced growth of new species.     

付老文泡湿地贴地气层中CO_2日平均浓度沿环境梯度的空间分异特征

以付老文泡湿地为研究区,在典型样带内设置具有不同环境梯度的六个观测区,研究了样带内贴地气层CO2日平均浓度的空间分异特征。结果表明,付老文泡湿地在7月份的贴地气层CO2日平均浓度较低,总平均值为264.14μmol/mol;付老文泡湿地最大CO2日平均浓度出现在近地面层,CO2日平均浓度由近地面层向上呈现下降趋势。在四个高度水平上,CO2日平均浓度的水平分异特征明显,高值区和低值区分别出现在洼地和高地。在水分梯度作用下,洼地区内CO2日平均浓度在四个高度水平上均表现为样地A<样地B<样地C,且在垂直方向上均呈现出由近地层向上呈先减后增再骤然减少的变化趋势;样地D和样地E的CO2日平均浓度在垂直方向上变化趋势一致,由近地层向上呈现逐渐减少的变化趋势;而样地F的CO2日平均浓度的垂直变化不明显。     

高效液相色谱法测定酚类化合物

根据《水和废水监测分析方法》第4版测定水中酚类化合物,通过不同淋洗梯度试验,对不同淋洗梯度对出峰时间的影响作了探讨。     

Evaluation of a fetus at risk for dihydropteridine reductase deficiency by direct mutation analysis using denaturing gradient gel electrophoresis

Dihydropteridine reductase (DHPR) is an enzyme involved in the recycling of tetrahydrobiopterin (BH₄), which is an obligate co-factor of the aromatic amino acid hydroxylases. DHPR deficiency is a rare, autosomal recessive disorder caused by mutations in the QDPR gene. DHPR-deficient patients are diagnosed by a lack of response to a low phenylalanine diet and by severe neurological symptoms. Final diagnosis is made by measurements of neurotransmitters and pterin metabolites in cerebrospinal fluid (CSF) and urine, in addition to DHPR enzyme activity, which can be assessed in whole red blood cells. Treatment of DHPR deficiency can be difficult and the outcome is not always satisfying, even if all treatment strategies are followed. Therefore prenatal diagnosis is of great importance in affected families. Prenatal diagnosis is possible by measuring DHPR activity in different cell types but this is time consuming. More than 25 different mutations have to date been identified in the QDPR gene and direct identification of a mutation in a fetus would be easy and rapid. We have developed a method based on denaturing gradient gel electrophoresis (DGGE) for the analysis of the QDPR gene. The method is useful for rapid and simultaneous scanning of all exons and flanking intronic sequences of the QDPR gene. We describe the first prenatal diagnosis conducted using this method. Copyright © 2001 John Wiley & Sons, Ltd.     

Diversity of methanotrophs in Zoige wetland soils under both anaerobic and aerobic conditions

Zoige wetland is one of the most important methane emission centers in China. The oxidation of methane in the wetland a ects global warming, soil ecology and atmospheric chemistry. Despite their global significance, microorganisms that consume methane in Zoige wetland remain poorly characterized. In this study, we investigated methanotrophs diversity in soil samples from both anaerobic site and aerobic site in Zoige wetland using pmoA gene as a molecular marker. The cloning library was constructed according to the pmoA sequences detected. Four clusters of methanotrophs were detected. The phylogenetic tree showed that all four clusters detected were a liated to type I methanotrophs. Two novel clusters (cluster 1, cluster 2) were found to relate to none of the recognized genera of methanotrophs. These clusters have no cultured representatives and reveal an ecological adaptation of particular uncultured methanotrophs in Zoige wetland. Two clusters were belonging to Methylobacter and Methylococcus separately. Denaturing gradient gel electrophoresis gel bands pattern retrieved from these two samples revealed that the community compositions of anaerobic soil and aerobic soil were di erent from each other while anaerobic soil showed a higher metanotrophs diversity. Real-time PCR assays of the two samples demonstrated that aerobic soil sample in Zoige wetland was 1.5 times as much copy numbers as anaerobic soil. These data illustrated that methanotrophs are a group of microorganisms influence the methane consumption in Zoige wetland.     

Soil-profile distribution of carbon and associated properties in no-till along a precipitation gradient in the central Great Plains

No-till (NT) farming is considered as a potential strategy for sequestering C in the soil. Data on soil-profile distribution of C and related soil properties are, however, limited, particularly for semiarid regions. We assessed soil C pool and soil structural properties such as aggregate stability and strength to 1 m soil depth across three long-term (≥21 year) NT and conventional till (CT) experiments along a precipitation gradient in the central Great Plains of the USA. Tillage systems were in continuous winter wheat (Triticum aestivum L.) on a loam at Hutchinson and winter wheat-sorghum [Sorghum bicolor (L.) Moench]-fallow on silt loams at Hays and Tribune, Kansas. Mean annual precipitation was 889 mm for Hutchinson, 580 mm for Hays, and 440 mm for Tribune. Changes in profile distribution of soil properties were affected by differences in precipitations input among the three sites. At Hutchinson, NT had 1.8 times greater SOC pool than CT in the 0-2.5-cm depth, but CT had 1.5 times greater SOC pool in the 5-20-cm. At Hays, NT had 1.4 times greater SOC pool than CT in the 0-2.5-cm depth. Differences in summed SOC pool for the whole soil profile (0-1 m depth) between NT and CT were not significant at any site. The summed SOC pool with depth between NT and CT were only significant above the 5 cm depth at Hutchinson and 2.5 cm depth at Hays. At Hutchinson, NT stored 3.4 Mg ha⁻¹ more SOC than CT above 5 cm depth. At Hays, NT stored 1.35 Mg ha⁻¹ more SOC than CT above 2.5 cm depth. Moreover, NT management increased mean weight diameter of aggregates (MWDA) by 3 to 4 times for the 0-5-cm depth at Hutchinson and by 1.8 times for the 0-2.5-cm depth at Hays. It also reduced air-dry aggregate tensile strength (TS) for the 0-5-cm depth at Hutchinson and Hays and for the 0-2.5-cm depth at Tribune. The TS (r = −0.73) and MWDA (r = 0.81) near the soil surface were more strongly correlated with SOC concentration at Hutchinson than at Hays and Tribune attributed to differences in precipitation input. Results suggested NT impacts on increasing SOC pool and improving soil structural properties decreased with a decrease in precipitation input. Changes in soil properties were larger at Hutchinson (880 mm of precipitation) than at Hays and Tribune (≤580 mm). While NT management did not increase SOC pool over CT for the whole soil profile, the greater near-surface accumulation of SOC in NT than in CT was critical to the improvement in soil structural properties. Overall, differences in precipitation input among soils appeared to be the dominant factor influencing NT impacts on soil-profile distribution of SOC and soil structural properties in this region.