Roles of acid-producing bacteria in anaerobic digestion of waste activated sludge

Three acid-producing strains, AFB-1, AFB-2 and AFB-3, were isolated during this study, and their roles in anaerobic digestion of waste activated sludge (WAS) were evaluated. Data of 16S rRNA method showed that AFB-1 and AFB-2 were Bacillus coagulans, and AFB-3 was Escherichia coli. The removal in terms of volatile solids (VS) and total chemical oxygen demand (TCOD) was maximized at 42.7% and 44.7% by inoculating Bacillus coagulans AFB-1. Besides, the optimal inoculum concentration of Bacillus coagulans AFB-1 was 30% (v/v). Solubilization degree experiments indicated that solubilization ratios (SR) of WAS reached 20.8%±2.2%, 17.7%±1.48%, and 11.1%±1.53%. Volatile fatty acids (VFAs) concentrations and compositions were also explored with a gas chromatograph. The results showed that VFAs improved by 98.5%, 53.0% and 11.6% than those of the control, respectively. Biochemical methane potential (BMP) experiments revealed that biogas production increased by 90.7% and 75.3% when inoculating with Bacillus coagulans AFB-1 and AFB-2. These results confirmed that the isolated acid-producing bacteria, especially Bacillus coagulans, was a good candidate for anaerobic digestion of WAS.

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草甘膦与镉复合胁迫对玉米幼苗抗氧化酶活性及光合作用的影响

为了探讨草甘膦(PMG)与重金属镉(Cd)复合胁迫对作物(玉米幼苗)生长的影响作用机制。通过温室盆栽试验,分别进行了不同浓度的PMG单一处理(浓度分别设计为0、1.25、2.5、5、10、20 mg·kg~(-1))和不同浓度的PMG(浓度分别为0、1.25、2.5、5、10、20 mg·kg~(-1))与浓度5 mg·kg~(-1)Cd2+的复合处理。采用分光光度法和连续激发式荧光仪分别对玉米幼苗抗氧化酶(过氧化物酶POD、过氧化氢酶CAT、超氧化物歧化酶SOD)、丙二醛(MDA)、叶绿素含量、荧光动力学曲线及相关参数进行了测定。结果表明,单一和复合胁迫分别在PMG浓度为1.25~5 mg·kg~(-1)、1.25~2.5 mg·kg~(-1)时,玉米幼苗通过增大抗氧化酶(SOD、POD、CAT)活性,清除积累过多的活性氧自由基,提高叶绿素含量的合成,加大光合作用速率,促进玉米幼苗的生长;单一和复合胁迫分别在PMG浓度为5~20 mg·kg~(-1)、2.5~20 mg·kg~(-1)时,由于玉米幼苗积累了过多的膜脂过氧化物,导致抗氧化系统损坏,阻碍叶绿素含量的合成,同时也损害了PSII的功能(MO、φPO、ΨO、φEO、φDO、ABS/RC、TRO/RC、ETO/RC、DIO/RC、PIABS),导致玉米幼苗光合作用受到抑制,阻碍幼苗的生长。研究表明,草甘膦单一胁迫和与重金属镉复合胁迫,对玉米幼苗酶活性及光合作用的影响,均随处理浓度的升高表现为双阶段性,低浓度促进,高浓度抑制;与同浓度的PMG单一处理相比,Cd2+的存在,加大了PMG单独存在时的损害作用,使得玉米幼苗对PMG胁迫的敏感浓度点从5 mg·kg~(-1)降低到2.5 mg·kg~(-1)。     

洱海流域湖泊湖滨带福寿螺时空分布

福寿螺是世界100种恶性入侵物种中唯一的水生螺,已对大理及周边地区造成了不可估量的经济损失和生态安全问题。为探究洱海流域湖泊湖滨带福寿螺时空分布及与水环境因子、季节之间的关系,探索福寿螺在大理地区的入侵机制,为大理地区高效防治福寿螺提供建设性建议,并为福寿螺时空分布格局的相关研究积累资料,于2016年冬季和2017年夏季在大理洱海及其上游水源地海西海、西湖、茈碧湖、绿玉池,以及罗时江湿地进行系统抽样,利用统计软件分析福寿螺分布与水质关系,结合GIS,分析福寿螺的时空分布以及潜在入侵危害。结果表明,从空间尺度上,洱海流域福寿螺有进一步扩散的趋势;从时间尺度上,福寿螺的密度随季节性水位的改变而变化;洱海流域的福寿螺分布和水质因子之间基本无相关性。     

微囊藻毒素-LR对雄性黑斑蛙精巢中CYP46A1,CYP2H2和CYP2G1 mRNA表达的影响

微囊藻毒素-LR(microcystin-LR,MC-LR)是分布最广泛和毒性最强的一种微囊藻毒素,对水生动物造成潜在的健康威胁。大量科学研究证实,动物体中的细胞色素P450酶(CYP)参与内源性物质及外源毒性物质的代谢过程。为探究两栖动物生殖器官中的CYP酶对低剂量MC-LR生殖毒效应的调节作用,选择雄性黑斑蛙(Rana nigromaculata)为受试动物,采用静态置换法和体内暴露方法,分别暴露于0、0.1、1和10μg·L~(-1)MC-LR溶液0、7和14 d;用实时荧光定量PCR方法检测精巢中CYP46A1、CYP2H2和CYP2G1的mRNA表达水平。结果表明,暴露于0.1、1和10μg·L~(-1)MC-LR 14 d后,CYP46A1在mRNA水平分别上调了1.86、1.65和1.22倍,CYP2H2在mRNA水平分别上调了4.62、1.80和1.04倍,CYP2G1的mRNA水平分别上调了2.63、2.16和1.56倍。MC-LR在1μg·L~(-1)剂量下暴露7 d后,CYP46A1、CYP2H2和CYP2G1 mRNA水平均出现显著上调。上述研究表明,微囊藻毒素对黑斑蛙精巢3种CYP基因在mRNA水平上都存在低剂量刺激效应。低剂量MC-LR能诱导黑斑蛙精巢中CYP46A1转录水平变化,促进胆固醇转化为24S-羟化胆固醇,潜在破坏雄性黑斑蛙精巢中胆固醇水平的平衡; MC-LR也能够诱导精巢中CYP2H2和CYP2G1转录水平的变化,潜在调节CYP2H2和CYP2G1转录水平,进而影响MC-LR的代谢作用。     

滨海滩涂不同围垦年代垦区农作物重金属累积特征及其与氮、磷的关系

为探明滨海滩涂围垦区农作物重金属累积特征及其与围垦年代、作物氮磷含量及化学计量比的关系,采集盐城地区不同围垦年代(围垦20、30、40、60年)农田4种主要作物(大麦、小麦、油菜、蚕豆)样品63个,测定了其根、茎叶和籽粒中Cd、Cu、Zn、Pb、Hg、As及全氮(N)、全磷(P)和粗蛋白(CP)含量,分析了重金属累积特征及与围垦年代、N、P、CP及N/P比的关系,并采用单因子污染指数法和内梅罗综合污染指数法对重金属污染程度和安全水平进行了评价。结果表明,1)围垦农田作物整株各指标含量分别为Cd (0.52±0.94)、Cu (12.98±16.00)、Zn (34.93±27.91)、Pb (3.50±5.88)、Hg (0.0063±0.0063)、As (1.94±3.72) mg·kg~(-1)及N(13.69±8.27)、P (5.98±2.24)、CP (79.55±49.54) g·kg~(-1);籽粒中则分别为(0.0059±0.020)、(1.83±1.48)、(11.13±4.45)、(0.09±0.30)、(0.0023±0.0036)、(0.0021±0.0048) mg·kg~(-1)及(19.21±7.68)、(6.04±1.64)、(111.78±47.81) g·kg~(-1); 2)作物重金属均表现为根茎叶籽粒,N和CP与之相反,表现为根茎叶籽粒,而P则表现为根籽粒茎叶; 3)不同围垦年代之间作物重金属、N、P、CP含量、N/P比及综合污染指数(Pz)均没有显著差异(P0.05); 4)各作物籽粒6种重金属单因子污染指数均值均小于1,除个别样品Pb超标(超标率11%)外,其他重金属均未超标; 5)作物籽粒重金属Pz均值为0.38,表明该地区作物重金属总体处于安全级,但大麦、小麦、油菜籽粒均有样品Pb含量超过警戒线,个别样品甚至达到重度污染水平; 6)作物整株各重金属之间、重金属与P之间均存在显著正相关(P0.01),而重金属与N、CP、N/P存在显著负相关(P0.01),在籽粒中则相关性均不显著(P0.05)。以上结果显示,盐城滨海滩涂围垦区作物重金属累积与围垦时间关系不大,其含量目前尚处于可接受范围内,但Pb污染值得关注,作物重金属与P之间存在一定的相互促进作用,而与N存在一定的拮抗作用,高氮低磷的机体养分状况有助于降低重金属含量。     

The origin of high hydrocarbon groundwater in shallow Triassic aquifer in Northwest Guizhou,China

Original high hydrocarbon groundwater represents a kind of groundwater in which hydrocarbon concentration exceeds 0.05 mg/L. The original high hydrocarbon will significantly reduce the environment capacity of hydrocarbon and lead environmental problems. For the past 5 years, we have carried out for a long-term monitoring of groundwater in shallow Triassic aquifer in Northwest Guizhou, China. We found the concentration of petroleum hydrocarbon was always above 0.05 mg/L. The low-level anthropogenic contamination cannot produce high hydrocarbon groundwater in the area. By using hydrocarbon potential, geochemistry and biomarker characteristic in rocks and shallow groundwater, we carried out a comprehensive study in Dalongjing (DLJ) groundwater system to determine the hydrocarbon source. We found a simplex hydrogeology setting, high-level water–rock–hydrocarbon interaction and obviously original hydrocarbon groundwater in DLJ system. The concentration of petroleum hydrocarbon in shallow aquifer was found to increase with the strong water–rock interaction. Higher hydrocarbon potential was found in the upper of Guanling formation (T₂g³) and upper of Yongningzhen formation (T₁yn⁴). Heavily saturated carbon was observed from shallow groundwater, which presented similar distribution to those from rocks, especially from the deeper groundwater. These results indicated that the high concentrations of original hydrocarbon in groundwater could be due to the hydrocarbon release from corrosion and extraction out of strata over time.

     

Changes in CO2 flux for different recovery processes of desertification in the alpine meadows of Northwest Sichuan北大核心CSCD

Desertification has emerged as a serious threat to the alpine meadows of Northwest Sichuan in recent decades. Artificial vegetation had certain effects on desertification recovery, while how the CO2 flux changed and its reasons are still unclear. During the growing season in 2016 (i.e., from July to September), we selected the desertified alpine meadows with different recovery degrees, including the early stage of restoration, the middle stage of restoration, the late stage of restoration, and control (the unrecovered desertification meadow) as four transects. CO2 flux was measured by the instrument LI-8100, and the microenvironment factors that affected CO2 flux changes were analyzed. The results showed that the carbon sequestration function of desertified alpine meadows gradually increased with the degree of recovery. Net ecosystem exchange (NEE) were -1.61, -3.55, and -4.38 μmol m-2 s-1 in the early, mid-term, and late transects, respectively, and the most dramatic changes occurred from the early stage to mid-term stage, increasing by 120.50%. Both ecosystem respiration (ER) and soil respiration (SR) were enhanced significantly with restoration (P < 0.05). In mid or late July, NEE, ER, and SR reached their maximum values, and thereafter, the indicators varied to near zero (P < 0.05). During the whole growing season, the daily dynamic in CO2 flux for the control alpine meadow was mild and retained the trend of continuous release all day, but that in the desertified alpine meadow was a single peak pattern. Moreover, with restoration process, the peak of CO2 flux increased and reached a peak in the late stage of the recovery process. The regression analysis showed that there was a significant positive correlation between CO2 flux and vegetation coverage, aboveground biomass, and soil moisture (0-5 cm) (P < 0.01), and a weak correlation with 0-5-cm soil temperature (P < 0.01). This indicates that topsoil moisture (5 cm) is a more significant factor for CO2 flux than topsoil temperature during the growing season in the restoration of desertified alpine meadows in Northwest Sichuan. In general, the vegetation recovery significantly improved the carbon-sequestration ability of the desertified alpine meadows during the growing season in Northwest Sichuan, and at the middle stage of restoration, the carbon-sequestration ability improved significantly due to vegetation restoration and increase in topsoil (0-5 cm) moisture. © 2018 Science Press. All rights reserved.     

Effects of water velocity on bulk water quality and biofilm population structure in drinking water distribution systems北大核心CSCD

To study the effect of flow velocity on drinking water distribution systems, bulk water quality was monitored over 28 days, biomass was measured, and 16S rDNA was sequenced on the 28th day using a water distribution simulation system. The relationship between bulk water quality and biofilm was statistically analyzed. Flow velocity of 0.5 m/s yielded the most total organic carbon (TOC) (5.26 ± 0.17 mg/L) in the bulk water, the most bulk water bacteria (lg (n+1/mL-1) = 4.79 ± 0.02), the worst bulk water quality, and the most biofilm bacteria (lg (n+1/cm-2) = 5.48 ± 0.06). A Pearson correlation analysis showed the total number of biofilm bacteria was positively correlated with conductivity (R = 0.73, P < 0.01), turbidity (R = 0.87, P < 0.001), TOC (R = 0.94, P < 0.001), and total bacteria (R = 0.92, P < 0.001), and was negatively correlated with residual chlorine (R = -0.68, P < 0.05). Biofilm diversity was high under the low (0.1 m/s) and high (2.5 m/s) flow rates, but the bacterial diversity of biofilm was the lowest at the 0.5 m/s flow rate, in which Proteobacteria dominated the biofilm community structure. These results suggest that flow velocity affects bulk water quality and biofilm population structure, and water quality and biofilm population structure are interrelated, which provides the theoretical basis for research on biofilms in drinking water distribution systems. © 2018 Science Press. All rights reserved.     

Mycelial culture of wild Inonotus hispidus parasitizing the jujube tree and the cultivation conditions of its fruit body on rice medium北大核心CSCD

Inonotus hispidus is a kind of rare medicinal fungus, and its natural resources are very scarce. Currently, the artificial cultivation technology of I. hispidus is not completely developed, and this reflects on its extremely low biological conversion rate and long cultivation period. In order to improve the bioconversion rate and shorten the production cycle of I. hispidus, we first analyzed the mycelia culture conditions of the collected I. hispidus, and then we further explore the method of domesticated cultivation of its fruiting body in rice medium. During the process of mycelial culture, the suitable temperature, pH, carbon source, and nitrogen source for mycelial growth were selected using the mycelial growth rate as index. During the domesticated cultivation of the fruiting body, the suitable culture medium for its growth was selected using the bioconversion rate as index. Screening results of mycelial culture conditions showed that the optimal culture conditions for the growth of mycelium of the wild I. hispidus were: temperature of 25 °C, initial pH of 6.0, glucose as the carbon source, and yeast extract powder as the source of nitrogen. The results of the domesticated cultivation showed that the biotransformation rate of I. hispidus was higher when using rice as the main medium substrate. The optimal cultivation conditions were: a 0.2% yeast extract content in the nutrient solution, a 1:1.6 ratio of rice to nutrient solution, and a 4 mL inoculum of the liquid strain. Under these conditions, it took about 4 days for the mycelium to grow over the cultivation medium. The time required for the differentiation of the primordium to form fruit bodies was about 20 days, and the bioconversion rate reached 28.70% ± 5.05%. The results of this study indicate the feasibility of using rice as the main substrate for the cultivation of I. hispidus, and it also provide new insights for the finding of new cultivation substrates for other rare medicinal fungi. © 2018 Science Press. All rights reserved.     

Carbon dioxide and methane emission from subsurface peatlands and its controlling factors北大核心CSCD

Peatland is an efficient carbon dioxide (CO2) sink on the continent and plays an important role in global carbon cycle. Climate change and human activities, two of the notable global environmental issues, have accelerated the degradation of peatlands during recent years. Global warming will increase the rate of aerobic decomposition in the surface of peatlands. Carbon stored in the subsurface of peatlands will be metabolized if the climatic conditions become favorable for decomposition. This study reviewed the carbon circle of subsurface peatland in natural environment and in environments disturbed by human activity or climate change. Furthermore, the major factors (environmental and human factors) that affect the carbon cycle were also discussed. According to a previous study, subsurface peatland will rapidly participate in the carbon cycle when the peatland is degraded. Water level, vegetation, and temperature were the main natural factors affecting the carbon cycle, whereas drainage, farming, and grazing were the main anthropogenic factors. Further studies should focus on different soil layer carbon dynamics, inorganic carbon content, and conservation and restoration of peatlands. The study methods should be a combination of macro with micro scale and focus on developing deep peat research techniques. Most of the previous studies focused on greenhouse gas emission and their response factors in short-term experiments. Thus, the mechanism and process of subsurface carbon are not clear and needs further study. © 2018 Science Press. All rights reserved.