甲醇对土壤甲烷氧化的影响及其微生物学机理

对设施栽培土壤甲烷氧化及其微生物学机理进行了研究，结果表明，不同土壤对甲烷的氧化能力各异，这可能与土壤的理化性质有关。土壤微生物是甲烷氧化的主要生物类群，不同碳源对甲烷氧化的影响各异，纤维素对甲烷氧化的抑制作用最小，高浓度的甲醇则对甲烷氧化具有强烈的抑制作用，而适当浓度的甲醇可极大地促进土壤甲烷的氧化。在甲烷释放极少的设施栽培土壤中，兼性营养甲烷氧化菌可能在甲烷氧化中占据主导地位。     

Factors affecting simultaneous nitrification and denitrification in an SBBR treating domestic wastewater

An aerobic sequencing batch biofilm reactor (SBBR) packed with Bauer rings was used to treat real domestic wastewater for simultaneous nitrification and denitrification. The SBBR is advantageous for creating an anoxic condition, and the biofilm can absorb and store carbon for good nitrification and denitrification. An average concentration of oxygen ranging from 0.8 to 4.0 mg/L was proved very efficient for nitrification and denitrification. Volumetric loads of TN dropped dramatically and effluent TN concentration increased quickly when the concentration of average dissolved oxygen was more than 4.0 mg/L. The efficiency of simultaneous nitrification and denitrification (SND) increased with increasing thickness of the biofilm. The influent concentration hardly affected the TN removal efficiency, but the effluent TN increased with increasing influent concentration. It is suggested that a subsequence for denitrification be added or influent amount be decreased to meet effluent quality requirements. At optimum operating parameters, the TN removal efficiency of 74%–82% could be achieved.     

镉对稻田土壤典型微生物种的胁迫生理毒性

以水稻田土壤中典型的单种微生物为实验材料,采用纯培养方法,从个体水平上全面探讨了重金属镉胁迫对稻田土壤典型微生物的的生长、活性以及生化过程的生理毒性影响。研究表明:不同微生物纯培养对镉胁迫的敏感程度不同,G 较G-对Cd2 更为敏感,表现为世代时间缩短,最高菌浓度下降。固氮菌对Cd2 非常敏感,当Cd2 质量浓度为0.2mg·L-1时即完全抑制菌体增殖。同时,外源镉强烈的抑制作为稻田土壤中功能微生物的厌氧固氮菌及产甲烷细菌的生物活性,各菌种镉胁迫下细菌细胞内可溶性蛋白、还原糖、核酸质量浓度都在低质量浓度镉胁迫时有所增加;随着镉质量浓度的增加,细菌细胞内各种物质的质量浓度开始减小,以减慢细胞代谢速度,增强对镉胁迫的适应力;各种物质的质量浓度变化趋势为可溶性蛋白>还原糖>核酸,R.eutrophaDKC1细胞内含物质量浓度基本保持稳定。结果可在一定程度上说明镉对微生物的毒性效应,且能在早期较灵敏地指示污染的影响,作为稻田土壤环境受到污染胁迫的细胞生化指标具有一定可行性。     

环戊酮和环己酮的微生物降解途径、相关酶和基因研究进展

简略介绍了环戊酮和环己酮的应用及危害,综述了目前国内外在环戊酮和环己酮微生物降解方面的研究进展.具体介绍了环戊酮和环己酮降解代谢的过程及其相关的酶类和编码这些酶的基因,重点阐述了环戊酮1,2-单加氧酶和环己酮1,2-单加氧酶及其编码基因.图4参19     

乌江流域县域社会经济发展的综合评价与分析

在简要阐述了县域社会经济发展综合评价原则的基础上,建立了悬域社会经济发展综合评价的指标体系,利用层次分析法确定了各评价因子的权重。接着以乌江流域为例,对流域内４０个县域的社会经济发展水平进行了定量评价,指出了流域内县域社会经济发展中存在的问题,并提出了相应的对策,旨在为促进乌江流域的县域社会经济协调发展提供某些科学依据。     

唐山地震中人员伤亡情况的分析及若干启示

唐山大地震对人的伤害是立体的,人员伤亡的主要原因是房屋建筑的倒塌．唐山市区被废墟埋压者中有约84％的人活了下来．唐山地震中人员伤亡情况的分析,对如何减少地震伤亡以及有效开展救灾活动,提供了有益经验。     

黄土高原地区水资源合理利用

黄土高原地区自然资源丰富，但生态环境脆弱。区内既有巨大的开发任务，又有严重的环境整治问题，它们都需要大量的供水。该区地处干旱半干旱地区，水资源较贫乏，供需矛盾尖锐。针对地区水资源特征及需水特点，本文提出了水资源开发利用以节水与开发结合，开发利用与保护并重的措施，确保水资源能得到永续利用。     

Assessment of global industrial-age anthropogenic arsenic contamination

Arsenic, a carcinogenic trace element, threatens not only the health of millions of humans and other living organisms, but also global sustainability. We present here, for the first time, the global industrial-age cumulative anthropogenic arsenic production and its potential accumulation and risks in the environment. In 2000, the world cumulative industrial-age anthropogenic arsenic production was 4.53 million tonnes. The world-wide coal and petroleum industries accounted for 46% of global annual gross arsenic production, and their overall contribution to industrial-age gross arsenic production was 27% in 2000. Global industrial-age anthropogenic As sources (as As cumulative production) follow the order: As mining production >As generated from coal >As generated from petroleum. The potential industrial-age anthropogenic arsenic input in world arable surface in 2000 was 2.18 mg arsenic kg^–1, which is 1.2 times that in the lithosphere. The development of substitute materials for arsenic applications in the agricultural and forestry industries and controls of arsenic emissions from the coal industry may be possible strategies to significantly decrease arsenic pollution sources and dissipation rates into the environment.     

Comparison of Black Carbon,Total Organic Carbon,and PAH Concentrations in Surface Sediments from Two Main Rivers in Henan Province,China

Black carbon (BC) in surface sediments from Henan section of Yellow River and Huaihe River, China, was determined. Average content of BC in Huaihe River was 0.33%, higher than that in Yellow River (n?=?23) with mean value of 0.15%. Distribution patterns of BC in Yellow River and Huaihe River were similar, namely that tributaries had higher BC content than main stream. In addition, BC content in the mainstream of Yellow River and Huaihe River decreased with altitude. The BC content presented a significant positive correlation with clay (r?=?0.672; p?<?0.01) content in Yellow River, while neither did in Huaihe River. The ratio of BC/TOC ranged from 1.8–57.4% (median 29.6%), evidencing pyrogenic fossil fuel source of BC in Yellow River. Relatively low values of BC/TOC in Huaihe River (5.3%–28.8%, median 7.5%,) reflected that the origin of BC is from burning of biomass. In addition, Pearson rank correlation analysis showed that BC was in strong correlation with lighter PAH in Yellow River, while BC was in significant correlation with heavier PAH in Huaihe River. The ratio of BC/TOC indicated that BC in Yellow River mainly came from fossil fuel combustion, while BC in Huaihe River was primarily from biomass burning.