丹江口水库浮游细菌和氮磷循环基因垂直分布特征及其驱动因素

丹江口水库作为南水北调中线工程水源地,不同深度浮游细菌群落组成、 氮磷循环功能及其驱动因素尚未清晰. 选取丹江口水库5个生态点位,采用宏基因组学研究表层、 中层和底层垂直分布浮游细菌群落组成,分析预测氮磷循环功能及其驱动因素. 结果表明,丹江口水库主要由变形菌门、 放线菌门和浮霉菌门等优势种群组成,不同深度来源的浮游细菌群落结构具有显著差异,水温（T）、 氧化还原电位（ORP）、 溶解氧（DO）和Chla是影响浮游细菌群落组成的主要因素. 氮循环功能基因分析表明,主要涉及生物固氮过程、 硝化作用、 反硝化作用和异化硝酸盐还原作用等7个主要途径的gltB、 glnA、 gltD、 gdhA和NRT等39个氮循环功能基因. 磷循环功能基因分析表明,主要涉及有机磷矿化、 无机磷溶解、 调节等6个主要途径的pstS、 ppx-gppA、 glpQ和ppk1等54个磷循环功能基因. 聚类分析表明不同深度是影响氮磷循环功能基因组成和丰度的主要因素,表层和底层氮磷循环功能基因丰度高于中层样品. 奇异球菌属、 嗜氢菌属、 Limnohabitans和棍状杆菌属等是氮磷循环的关键物种. DO、 pH、 T、 总溶解性固体（TDS）、 电导率（EC）和Chla与氮磷循环功能基因显著相关,以上环境因子随丹江口水库深度增加浓度降低或升高,导致浮游细菌氮磷循环功能基因呈明显的垂直分布特征. 通过揭示丹江口水库不同深度浮游细菌群落组成、 氮磷循环功能及其影响因素,可为丹江口浮游细菌生态功能和多样性保护发挥潜在的作用.     

压裂返排液循环利用技术的应用

开发了压裂返排液"水质调节—混凝沉淀—精细过滤"处理工艺.将返排液pH调为7.8～8.0,采用无机铝盐混凝剂+有机阳离子高分子絮凝剂+沉淀剂(FJ-3)处理,采用20μm有机滤膜对混凝沉淀后水进行过滤处理,再经季铵盐类杀菌剂处理,出水再用于配制胍胶压裂液.无论是基液基础性能还是胶液耐温耐剪切能力以及破胶性能都与自来水配...     

附生假单胞菌存在下不同光照时间对铜绿微囊藻生长与磷代谢的影响

通过设置8/16、12/12、16/8不同光暗比,分析了附生细菌存在下不同光照时间对铜绿微囊藻(M icrocystis aeruginosa)生长及其与附生假单胞菌(Pseudom onassp.)磷代谢之间关系的影响。结果表明:光照时间越长,铜绿微囊藻生长越快,16 h光照下的比增长速率为8 h光照下的1.6倍。铜绿微囊藻的快速生长促进了附生细菌中磷的释放;藻细胞增殖越快,附生细菌释放的磷越多。铜绿微囊藻对数生长期末,8、12、16 h光照下附生细菌磷含量分别降至对数生长初期的87.8%、78.6%和64.9%。铜绿微囊藻对附生细菌磷释放的促进作用是由藻细胞生长对磷的消耗再吸收导致的。     

Nitrogen cycling of atmosphere-plant-soil system in the typical Calamagrostis angustifolia wetland in the Sanjiang Plain, Northeast China

The nitrogen (N) distribution and cycling of atmosphere-plant-soil system in the typical meadow Calamagrostis angustifolia wetland (TMCW) and marsh meadow Calamagrostis angustifolia wetland (MMCW) in the Sanjiang plain were studied by a compartment model. The results showed that the N wet deposition amount was 0.757 gN/(m2·a), and total inorganic N (TIN) was the main body (0.640 gN/(m2·a)). The ammonia volatilization amounts of TMCW and MMCW soils in growing season were 0.635 and 0.687 gN/m2, and the denitrification gaseous lost amounts were 0.617 and 0.405 gN/m2, respectively. In plant subsystem, the N was mainly stored in root and litter. Soil organic N was the main N storage of the two plant-soil systems and the proportions of it were 93.98% and 92.16%, respectively. The calculation results of N turnovers among compartments of TMCW and MMCW showed that the uptake amounts of root were 23.02 and 28.18 gN/(m2·a) and the values of aboveground were 11.31 and 6.08 gN/(m2·a), the re-translocation amounts from aboveground to root were 5.96 and 2.70 gN/(m2·a), the translocation amounts from aboveground living body to litter were 5.35 and 3.38 gN/(m2·a), the translocation amounts from litter to soil were larger than 1.55 and 3.01 gN/(m2·a), the translocation amounts from root to soil were 14.90 and 13.17 gN/(m2·a), and the soil (0-15cm) N net mineralization amounts were 1.94 and 0.55 gN/(m2·a), respectively. The study of N balance indicated that the two plant-soil systems might be situated in the status of lacking N, and the status might induce the degradation of C. angustifolia wetland.     

Imazaquin degradation and metabolism in a sandy loam soil amended with farm litters

Irnazaquin applied in legume crops has a long residual time in soil, which often impacts safety of the susceptible crops. To increase safety of imazaquin application, two composted litters, bovine manure （BM） and chicken manure （CM）, were used to determine their effects on imazaquin environmental behavior by incorporating each kind of manure into the tested sandy loam soil at 10% （w/w）. The degradation of imazaquin in BM- and CM-amended soil was about 2.4 and 1.5 times, respectively, faster than that in unamended soil. The half-lives of imazaquin in BM-amended soil varied between 6.7 and 15.4 d over the temperature range of 20 to 40℃, and the degradation rate constant （k） increased by a factor of about 1.5 for every 10℃ change. Higher mix ratio did not significantly increase the degradation, and the optimal active degradation of imazaquin was observed approximately at the mix ratio of 10：1 of soil to BM. The different moisture levels had negligible effect on imazaquin degradation. In both unamended and BM-amended treatments, two metabolites were observed at 5, 10 and 30 d after treatment. One metabolite at retention time （RT） of 8.4 rain was identified as 2-（4- hydroxyl-5-oxo-2-imidazolin-2-yl） quinoline acid, originating from the loss of isopropyl group and hydroxylation at the 4-position of imidazolinone ring. The other at RT of 12.9 rain was identified as quinoline-2,3-dicarboxylic anhydride, resulting from detachment of imidazolinone ring and the forming of dicarboxylic anhydride. This finding suggested that the addition of farm litters into soil might be a good management option since it can not only increase soil fertility but also contribute to increase safety of imazaquin application to the following susceptible crops.     

生态足迹研究现状及基于净初级生产力的计算方法初探

生态足迹是一种有效的再生资源更新能力的定量测度方法,其主要用于评估给定年,给定技术条件下生物圈的再生能力能否满足人类消费需求。本研究对国内外生态足迹模型的理论假设、生态足迹、生物承载力、生态盈余、生态赤字进行了简要介绍;在对国际组织发布的生态足迹报告以及生态足迹文献发表情况进行统计的基础上,回顾了国内外的生态足迹计算方法——基于净初级生产力的计算方法,并与现有的基于全球农业生态区的计算方法进行了比较,探讨了两种方法的优缺点;最后对生态足迹今后的研究重点提出了一些看法和展望。     

红壤稻田系统有机物循环再利用潜力及增产作用

10年田间试验结果表明：红墩妥田系统有机养分循环再利用潜力大，水稻收获，年均从稻田系统中输出NPK的总量最大可达到224.7,53.0和271.4kg/hm^2，有机物循环再利用，年均可归N，P，K量最大分别为115.1,35.8和231.5kg/hm^2，占系统输总量的51.2%,67.5%g和85.3%，保持稻田系统内有机物循环再利用可提高系统生产力，在不施化肥的情况下，增产3056kg/hm^2，增施N肥，增产2753kg/hm^2，增施N，P肥，增产1543kg/hm^2；NPK配合，增产984kg/hm^2；有机物循环再利用还可增强稻田系统的稳产性能，降低稻谷产量的年际变异系数；有机物循环再利用对水稻的增产有着明显的残效叠加作用，在施用N，P，K化肥基础上圾机物养分循环再利用水稻增产率在试验期间的前5年为7．2％，后5年平均为9．4％。     

降水量时间序列变化的小波特征

利用小波变换对降水量时间序列的多时间尺度变化及突变特征进行了探讨。小波变换不仅能将降水量时间序列的频率特征在时间域上展现出来，清晰地给出各种时间尺度的强弱和分布情况以及早涝变化趋势和突变点，而且还能分析出其主要周期。以新安江流域黄山地区主汛期(5—7月)和年降水量为例，计算表明，其年际及年代际时间尺度在时域中分布不均匀，具有明显的局部化特征；同时分析出主汛期降水具有8年、19年左右的周期，年降水存在6年、19年左右的周期；研究还表明，主汛期降水与年降水的时间尺度变化比较接近。     

干湿循环作用下白鹤滩小坝组红层砂岩强度特性与结构损伤研究

针对库岸消落带岩石长期处于干湿循环状态导致岩石劣化损伤威胁库岸稳定的工程问题,以白鹤滩水电站库区小坝组红层砂岩为研究对象,对不同干湿循环次数下“自然浸水”和“真空吸水”两种饱水方式的小坝组砂岩岩样进行单轴压缩试验、吸水试验、CT扫描试验、波速试验,研究了干湿循环作用下小坝组砂岩力学特性、空隙特性及损伤特性的变化规律。结果表明：干湿循环次数n相同条件下真空吸水砂岩岩样的强度参数普遍低于自然浸水砂岩岩样,砂岩的单轴抗压强度σ_c在干湿循环次数n为10～15次之间出现拐点;小坝组砂岩的总开空隙率n₀、大开空隙率n_b与n呈线性关系,大开空隙在砂岩强度劣化中起主要作用;随干湿循环的进行小坝组砂岩单轴抗压破裂面的分形维数增大;小坝组砂岩的纵波波速v_p、横波波速v_s与n的变化规律和σ_c与n的变化规律呈现出一致性,真空吸水加速,加深了砂岩强度劣化;定义了小坝组砂岩的纵向和横向损伤变量,干湿循环作用对砂岩的纵向损伤大于横向损伤。该研究结果可为白鹤滩大型水电工程库岸消落带岩体差...