Land-use history has a stronger impact on soil microbial community composition than aboveground vegetation and soil properties

The response of soil microbial communities following changes in land-use is governed by multiple factors. The objectives of this study were to investigate (i) whether soil microbial communities track the changes in aboveground vegetation during succession; and (ii) whether microbial communities return to their native state over time. Two successional gradients with different vegetation were studied at the W. K. Kellogg Biological Station, Michigan. The first gradient comprised a conventionally tilled cropland (CT), mid-succession forest (SF) abandoned from cultivation prior to 1951, and native deciduous forest (DF). The second gradient comprised the CT cropland, early-succession grassland (ES) restored in 1989, and long-term mowed grassland (MG). With succession, the total microbial PLFAs and soil microbial biomass C consistently increased in both gradients. While bacterial rRNA gene diversity remained unchanged, the abundance and composition of many bacterial phyla changed significantly. Moreover, microbial communities in the relatively pristine DF and MG soils were very similar despite major differences in soil properties and vegetation. After >50 years of succession, and despite different vegetation, microbial communities in SF were more similar to those in mature DF than in CT. In contrast, even after 17 years of succession, microbial communities in ES were more similar to CT than endpoint MG despite very different vegetation between CT and ES. This result suggested a lasting impact of cultivation history on the soil microbial community. With conversion of deciduous to conifer forest (CF), there was a significant change in multiple soil properties that correlated with changes in microbial biomass, rRNA gene diversity and community composition. In conclusion, history of land-use was a stronger determinant of the composition of microbial communities than vegetation and soil properties. Further, microbial communities in disturbed soils apparently return to their native state with time.     

一株分离自葛藤根际高效溶磷细菌特性研究及菌株鉴定

对分离自葛藤(Pueraria lobata L.)根际的一株高效溶磷细菌GTR15进行促生特性、主要生理生化指标测定和16S rDNA序列分析。结果表明,菌株GTR15的HD/CD值(溶磷圈直径HD,菌落直径CD)为2.22,28℃液体振荡培养7 d后对磷酸钙的溶解量为138.72 mg.L-1,分泌IAA(3-吲哚乙酸)及有机酸量分别为14.44 mg.L-1、46.00 mmol.L-1。菌株革兰氏染色为阴性,细胞短杆状;淀粉水解、吲哚、V-P(二乙酰试验)、苯丙氨酸脱氨酶、明胶液化及M-R(甲基红)试验呈阴性;柠檬酸盐、过氧化氢酶、硫化氢及硝酸盐还原等试验呈阳性,结合菌株16S rDNA序列分析结果,初步鉴定为肠杆菌(Enterobacter sp.)。该菌株在研制高效微生物磷肥接种剂方面可能具有较大潜力。     

基于6S模型的山区环境星影像大气校正研究

针对山区地形复杂,高程变化较大的特点,利用6S辐射传输模型建立查找表,结合研究区DEM对影像进行了大气校正。试验结果表明,校正后的影像清晰度、对比度提高了,消除了大气对NDVI的负面影响。     

铅锌矿区重金属污染对微生物数量及放线菌群落结构的影响

采集四川省汉源县富泉乡万顺铅锌矿区5个不同重金属浓度的土壤样品,进行了微生物数量及放线菌多样性的研究。经分离、纯化得到43株不同的放线菌,然后对其进行BOXAIR-PCR和16SrDNAPCR-RFLP分析。结果表明,铅锌矿区重金属复合污染对土壤微生物数量有较大的影响,随着铅锌矿区重金属污染程度的加剧,土壤微生物的总数下降。相关性分析表明,重金属含量与细菌数量呈极显著负相关（P〈0.01）,与放线菌数量、真菌数量呈显著负相关（P〈0.05）。供试菌株的16SrDNA用HaeⅢ、HinfⅠ和TaqⅠ酶切后具有32种遗传图谱类型。BOXAIR-PCR的聚类结果表明在86%的水平上,所有菌株分为10个遗传类型,结果基本与16SrDNAPCR-RFLP聚类差异不大。来源于高重金属的含量样品的菌株基本聚在一起,可能是重金属含量影响了放线菌的分布。同时,16SrDNA序列聚类分析结合系统发育树分析表明链霉菌属是汉源铅锌矿区主要的放线菌属并且具有遗传多样性。     

基于AT89S52和PID算法的温控系统

介绍了一种基于AT89S52单片机的温度控制系统,使用单总线温度传感器DS18B20检测温度,采用PID控制算法,分析系统原理,给出了系统的整体结构以及软件设计。实验结果表明,系统的稳定性比较好,精确度高。     

基于ZigBee和嵌入式技术的无线安防监控系统研究与设计

针对传统有线安防系统的局限性,通过对zigbee技术和嵌入式技术的研究,提出了一种基于zigbee组网技术和嵌入式控制技术的住宅小区无线安防监控系统,实现了布防后能够对住宅小区生活中存在的火灾、盗窃、煤气泄漏等安全隐患进行监测及报警。采用基于ZigBee标准的射频芯片CC2430,实现节点间数据的无线传输,并给出了系统的硬件原理框图和软件设计思路。     

水稻南方黑条矮缩病毒湖南鼎城株系S10片段的基因组序列分析

运用RT-PCR技术克隆了水稻南方黑条矮缩病毒（southern rice black-streaked dwarf virus,SRBSDV）湖南鼎城株系的基因组S10片段（SRBSDV-HuNDCS10）,并对其全序列进行了测定和生物信息学分析。结果显示,SRBSDV-HuNDC S10片段全长为1797bp（登录号：JQ337964）,含有1个ORF,编码557个氨基酸残基的衣壳蛋白,推测分子量约62.6kD,推测等电点为7.62,与已报道的广东、海南和云南分离物病毒的S10作比较,它们的核苷酸相似性分别为99.7%、99.0%和98.4%,氨基酸相似性分别为100.0%、99.5%和99.3%。对SRBSDV-HuNDCS10及部分Fijiviruses病毒对应片段在5＇URT与3＇URT存在的保守序列和互补序列进行了归纳,对其ORF编码的氨基酸序列进行了motif查找,得到该属（Fijiviruses）氨基酸序列的10个保守区段。此外,进行了糖基化位点、磷酸化位点及B细胞抗原表位预测,发现了3个可能的N端豆蔻酰基化位点,可能与病毒的侵染机制有关。     

Density separation of soil organic matter across three land uses in calcareous soils of Iran

ABSTRACT

The aim of this study was to examine the usefulness of physical and chemical fractionation in quantifying soil organic matter (SOM) in different stabilized fraction pools. Soil samples from three land use types in Lorestan province, Southwest Iran were examined to account for the amount of organic carbon and nitrogen in different SOM fractions. Size/density separation and chemical oxidation methods were applied to separate the SOM fractions including particulate organic matter (POM), Si + C (silt and clay), DOC (dissolved organic C), rSOM (oxidation-resistant organic carbon and nitrogen) and S + SA (sand and stable aggregates). The values obtained for TOC, TN, and HWC were highest in forest lands followed by the range and agricultural lands. Among the SOM fractions, S + SA showed the highest values (5.75, 5.77 and 20.6 g kg^?1 for agriculture, range and forest lands respectively) followed by POM, Si + C, rSOM, and DOC. The concentrations of C and N in the labile fractions obtained the higher values than in the stabilized fractions. Forest lands had the highest amounts of organic C and N among all fractions whereas agricultural lands showed highest values for inorganic C content of soils in different fractions.     

毛竹竹鞭内生细菌的特征及16S rDNA多样性分析

本研究利用传统的细菌分离方法,结合16S rDNA序列分析对毛竹竹鞭内生细菌的特征和多样性进行了分析。从福建省武夷山、将乐、长汀毛竹竹鞭中分离到34株内生细菌,初步归属于14属,20种。来源于不同地区的毛竹竹鞭内生细菌组成存在较大差异,其优势菌群为产碱杆菌属（Alcaligenes）和葡萄球菌属（Staphylococcus）。     

Community structure of bacteria on different types of mineral particles in a sandy soil

Various types of mineral particles in a soil probably provide different microenvironments for microorganisms. The purpose of this study is to investigate whether different types of mineral in a soil harbor different bacterial populations. DNA was extracted from five types (quartz, feldspar, pyroxene, magnetite, iron-coated reddish brown particles) of sand-size mineral particles separated from a sandy soil, and was amplified for partial 16 S rRNA gene by polymerase chain reaction (PCR). Twenty-nine to 69 amplicons per each type of mineral were cloned and sequenced, followed by phylogenetic affiliation of the sequences. As a result, some types of bacteria were detected on all of the types of mineral including the orders Rhizobiales, Bacillales, and Acidobacteriales. In the case of Acidobacteriales, higher percentages were found on magnetite and quartz. Some taxa were restricted to specific types of mineral; the class Actinobacteria was found on pyroxene but not on quartz, and rarely on magnetite and feldspar. Bacterial diversity at the order level estimated by Chao1 value was higher in feldspar and pyroxene than the other three types of mineral. The UniFrac Significance test indicated that the differences in bacterial communitiy structures among the particles were suggestive except that between feldspar and pyroxene. These results support the idea that different communities of bacteria were associated with each of the mineral types.