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991.
从我国内蒙古吉兰泰盐湖的样品中分离得到一株中度嗜盐细菌菌株JLT-01,研究了其形态和特性.结果显示:该菌株为杆状,革兰氏阴性,无芽孢,无荚膜,无鞭毛;最适培养温度为30℃,最适生长pH值7.5,最适生长盐度10%~12%(m/V),最适生长Mg2+浓度3.0%(m/V);能利用葡萄糖、蔗糖、半乳糖作为唯一碳源生长.脂肪酸成分分析表明在JLT-01中主要脂肪酸为C16:0与C18:1ω9c,含量分别为26.39%和20.30%.Tm法测定该菌的(G+C)含量(摩尔分数)为52.3%.以该菌的16S rRNA基因序列为基础构建了系统发育树;16S rRNA基因序列的序列同源性比对表明该菌与海杆菌属Marinobacter lipolyticus SM19T的同源性为98.0%,与Marinobacter属内其它菌株的同源性在96.0%~99.0%之间.DNA-DNA杂交实验分析显示:JLT-01与M.lipolyticus DSM15157的杂交率小于70%.结果表明,菌株JLT-01是海杆菌属的一个新菌株. 相似文献
992.
Concei??o Juana Fortes óscar Ferreira Paulo A. Silva Theo Moura Rui Capit?o Luís Amante Michalis Vousdoukas Maria Bezerra 《Journal of Coastal Conservation》2012,16(4):461-472
In the framework of a research project entitled ??BRISA??BReaking waves and Induced SAnd transport??, a methodology was devised to characterize the waves joining together in-situ measurements and numerical wave propagation models. With this goal in mind, a number of in-situ measurements were made, for selected positions in front of Praia de Faro (South Portugal), during four days (25th to 28th March, 2009) by using different types of equipments (e.g., resistive wave gauges, pressure sensors, currentmeters and a new prototype pore pressure sensor using optical fibre). Wave records were obtained simultaneously offshore (at a water depth of 11.7?m below mean sea level, MSL) and at the surf and swash zones. The data processing and analysis were made by applying classical time domain techniques. Numerical simulations of the wave propagation between offshore and inshore for the measurement period were performed with two numerical models, a 1D model based on linear theory and a nonlinear Boussinesq-type model, COULWAVE, both forced by the measured offshore wave conditions of 27th March 2009. Comparisons between numerical results and field data for the pressure sensors placed in the surf and swash zones were made and discussed. This approach enables to evaluate the performance of those models to simulate those specific conditions, but also to validate the models by gaining confidence on their use in other conditions. 相似文献
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In southern Taiwan, brooded larvae of Pocillopora damicornis and Seriatopora caliendrum are released year-round in synchrony with new moons, and each larval release occurs over multiple days. Using P. damicornis and S. caliendrum as a model system, we describe within-brood variation in larval phenotypes and test for release-day effects that influence larval performance in the pelagic phase. Research was conducted in 2010 using larvae from corals collected in June and July from Nanwan Bay (21°56.179??N, 120°44.85??E). In June, larval phenotypes of both species were characterized immediately following release, and their competency to settle assessed. In July, larvae of P. damicornis were collected on 3?days over the peak release period and incubated for 7?C11?days at 28.0?°C and 320???mol?quanta?m?2?s?1; their phenotypes and settlement competency were measured every 2?days. P. damicornis larvae released close to peak release were 1.6 times larger in size, contained twice the number of Symbiodinium larva?1, and were 44?% more likely to settle in the first 24?h than larvae released early in the brood. In addition, peak-release larvae respired at a lower rate than larvae released late in the brood. Similarly, S. caliendrum larvae released close to peak release were 1.4 times larger in size and were 33?% more likely to settle in the first 5?h than larvae released early in the brood. In July, P. damicornis larvae differed between early (2?days prior to peak), peak, and late (2?days after peak) release. Protein content of early-release larvae was lower than peak- and late-release larvae, and this difference persisted throughout the development. Further, release day affected the way larval respiration varied throughout development. By showing that brooded coral larvae differ between release days and display maternal effects influencing performance in the swimming phase, our results suggest that pocilloporid corals utilize bet-hedging to increase reproductive success. 相似文献
996.
在广泛收集整理相关资料和数据基础上,运用主成分分析法和GIS SuperMap技术对沈阳市2002—2010年大气污染物SO2、NO2、PM10年均值和8个环境监测站点2002—2010年的SO2、NO2、PM10年均值进行分析,结果表明:在时间变化方面,大气主要污染物的年均值在逐年下降,大气质量在近9年间逐渐转好,2007—2009年污染指数的月平均值变化曲线清晰呈现出两头高中间低的"U"字型变化趋势;在空间变化方面,从市中区到近郊区再到远郊区有逐渐减弱的趋势,市中心的太原街、小河沿的环境质量逐年转好,但市郊区的环境质量在逐年下降。 相似文献
997.
利用水解溶菌酶对从SBR系统中取出的部分污泥进行水解,然后再回流到SBR系统中,通过与未加水解溶菌酶的相同系统对比,研究了水解溶菌酶对SBR系统中污泥减量与污泥特性等方面的影响.结果表明,在连续50d的运行期间,水解溶菌酶作用下的SBR系统中剩余污泥减量总计达到76.29%,而该系统对COD与氨氮的降解效率与未加酶系统基本持平,分别为88.21%与68.72%,但其TP平均去除率较未加酶系统降低了17.2%;系统中由于水解溶菌酶的添加,污泥的微生物活性得到强化,比氧气吸收速率平均提高35%,ATP的平均值比对比系统提高了3.12nmol/mgMLSS. 相似文献
998.
紫外辐射光解与生物降解同步耦合的气升式内循环反应器用于喹啉的降解.实验过程中分别采用单独紫外光解、单独生物降解和紫外光解与生物降解同步耦合的方法对喹啉进行降解.结果表明,喹啉在紫外光解与生物降解同步耦合的作用下,其降解速率明显提高.喹啉降解动力学分析结果表明,喹啉的生物降解可以用有抑制性的Haldane模型描述.相比生物降解过程,单独紫外光解对喹啉的降解速率可以忽略,但将紫外辐射与生物降解耦合在一起后,可以提高喹啉的最大降解速率近1倍并减小抑制常数36%,同时还可以提高喹啉的矿化程度. 相似文献
999.
以简青霉Penicillium simplicissimum (Oudem.) Thom BGA为出发菌株,对其进行原生质体紫外诱变.经过筛选获得2株诱变菌株(J12与J18),它们的木质素降解酶酶活要明显高于出发菌株J.其中诱变菌株J12产生的漆酶和锰过氧化物酶酶活较高,相对于出发菌株J分别提高了145%和47%,达到44.0,50.9 U/g.诱变菌株J18产生的木质素过氧化物酶酶活较高,达到67.1 U/g,相对于出发菌株J提高了40%.且木质素降解率也最高,相对于出发菌株J分别提高了198.1%.经过7次传代, J12和J18的木质素降解酶活性保持稳定,没有降低. 相似文献
1000.
It is necessary to identify the hydrogeochemical processes and analyze the causes of groundwater pollution due to the lack of knowledge about the groundwater chemical characteristics and the endemic diseases caused by groundwater pollution in the northern Ordos Cretaceous Basin. In this paper, groundwater chemical facies were obtained using the piper trilinear diagram based on the analysis of 190 samples. The hydrogeochemical processes were identified using ionic ratio coefficient, such as leaching, evaporation and condensation. The causes and sources of groundwater pollution were analyzed by correspondence analysis, and the spatial distribution and enrichment reasons of fluoride ion were analyzed considering the endemic fluorosis emphatically. The results show that leaching, evaporation and condensation, mixing, and anthropogenic activities all had significant impact on hydrogeochemical processes in the study area. However, cation exchange and adsorption effects were strong in the S2 and S3 groundwater flow systems, but weak in S1. Groundwater is mainly polluted by Mn and CODMn in the study area. The landfill leachate, domestic sewage, and other organic pollutants, excessive use of pesticides and fertilizers in agriculture, and pyrite oxidation from long-term and large-scale exploitation of coal are the sources of groundwater pollution. The S1 has the highest degree of groundwater pollution, followed by S2 and S3. High concentration of fluoride ion is mainly distributed in the north and west of study area. Evaporation and condensation and groundwater chemistry component are the most important causes of fluoride ion enrichment. The results obtained in this study will be useful for understanding the groundwater quality for effective management and utilization of groundwater resources and assurance of drinking water safety. 相似文献