parDE基因对重组质粒pLM2在Enterobacter gergoviae 57-7中稳定性的影响

将 parDE基因克隆到载有组成型表达nifA基因的质粒 pST10 2 1上 ,得到重组质粒pLM2 .将 pLM2 ,pST10 2 1分别转到玉米联合固氮菌Enteorbactergergoviae 5 7 7(E5 7 7) ,获得转化子E5 7 7(pLM2 ) ,E5 7 7(pST10 2 1) ,二者在c(NH+ 4 ) =5 0mmolL-1的Kp培养基中表达的固氮活性一致 .将pLM2 ,pST10 2 1分别转到E .coliDH5α(pMGFP2 .1) ,培养物用 4 88nm光激发后在 5 10nm均有相同的的荧光特征发射峰 .上述实验表明 ,重组质粒pLM2仍保留了原质粒pST10 2 1中nifA的功能 .但质粒 pLM2和 pST10 2 1在E5 7 7中的稳定性试验表明 ,E5 7 7(pST10 2 1)在无抗生素的LB中继代培养 70代后 ,质粒几乎全部丢失 (仅存 1% ) ;而E5 7 7(pLM2 )继代培养 10 0代后 ,质粒全部存在 (10 0 % ) .图 4表 1参 12     

Seed treatment and inhibition of plantpathology by chitosan

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山东淄博玉米产区土壤砷含量空间变异研究

采用地统计及地理信息(GIS)技术研究了山东省淄博玉米产区土壤砷含量空间变异性及其分布特点.淄博玉米产区土壤砷监测数据呈正偏态分布,为实现数据集正态化及降低偏大值对预测结果的影响,对原始数据集进行了自然对数变换.结果表明,变换后数据集的经验半变异函数存在明显各向异性,在北偏东70°方向上变异性最弱.应用指数模型拟合经验半变异函数,采用普通克里格法预测砷元素的空间分布状况.研究表明,本区域土壤砷含量存在明显的空间异质性,污水灌溉是引起土壤砷元素空间变异最主要的因素,监测区内土壤As元素含量存在实际“亏损”状况.     

不同氮水平下间作对玉米土壤硝化势和氨氧化微生物数量的影响

利用荧光定量PCR(real-time quantitative PCR,Q-PCR)技术,结合氨氧化细菌(ammonia oxidizing bacteria,AOB)和氨氧化古菌(ammonia oxidizing archaea,AOA)丰度和土壤理化性质的测定,探索了不同氮水平下间作对玉米土壤硝化势(PNF)的影响.试验设置玉米单作和与马铃薯间作两个种植模式,4个施氮水平(不施氮N0、1/2常规施氮N1、常规施氮N2和3/2常规施氮N3)的随机区组试验.结果表明,从不施氮到常规施氮,土壤硝化势和AOA、AOB数量均随施氮量增加而逐渐增加,而高氮(N3)时与N2没有显著差异;间作对土壤硝化势、AOA与AOB数量的影响与施氮量和作物生育期有关,低氮投入(N1)间作有利于增加土壤氨氧化微生物数量和硝化作用.施肥是硝化势增加的主要驱动因子,相关性分析结果表明,土壤含水量是影响PNF的主要环境因子;PNF与土壤中AOA、AOB amoA基因丰度成显著的正相关.尽管玉米马铃薯间作降低了土壤中AOA、AOB amoA基因丰度,却使得间作土壤中AOB占据氨氧化微生物数量上的优势.以上结果表明,施氮和间作均影响了土壤硝化作用和氨氧化微生物AOA和AOB数量的变化,这些变化会影响土壤环境质量.     

晋南两熟半干旱区“粮药”(半夏)农田生态抗旱耕作模式效益研究

采用大田试验,设计冬小麦(Triticum aestivum Linn.)在春季起身后套作半夏[Pinellia ternata(Thunb.)Breit.](小麦/半夏)、冬油菜(Brassica campestris L.)收获后复播半夏[Pinellia ternata(Thunb.)Breit.](油菜-半夏)和春玉米(Zea mays L.)与半夏[Pinellia ternata(Thunb.)Breit.]间作(玉米+半夏)3种耕作模式,探讨晋南两熟半干旱区适宜半夏的粮药耕作模式。结果表明:与油菜-半夏、玉米+半夏耕作模式相比,小麦/半夏耕作模式经济产量最高,生态效益最好;不同半夏品种中,西河半夏(原产地温度相对最低)产量最高,新绛半夏(原产地温度相对较高)产量最低。表明半夏适宜于从低温地区引种到高温地区栽培,可提高产量。与商洛半夏和新绛半夏相比,西河半夏分别增产19.1%和41.9%;小麦/半夏耕作模式为最佳粮药耕作模式,其半夏产量与油菜-半夏和玉米+半夏耕作模式相比,分别增产53.4%和70.8%。     

土壤微生物群落对玉米根茬和茎叶残体碳的利用特征

以沈阳农业大学连续29a棕壤长期定位施肥试验为基础,以¹³C标记的玉米植株为试验试材,采用田间原位培养方法和磷脂脂肪酸-稳定同位素示踪联用（PLFA-SIP）技术,研究土壤不同粒级团聚体中微生物群落对残体碳的同化状况,及土壤有机碳的固定这一关键生物地球化学过程.结果表明：植物残体添加显著增加了全土及各粒级团聚体中各微生物群落PLFAs含量,其中以真菌PLFAs含量增幅最高,细菌中以革兰氏阴性菌含量增幅最高;但不同残体类型并未对全土中各群落PLFAs含量产生显著影响.茎叶碳与根茬碳的矿化率无显著差异;根茬碳对总PLFAs碳库的贡献是茎叶碳的3.9倍,说明根茬碳更有利于通过微生物合成的方式贡献于土壤有机碳库.残体碳占不同微生物群落PLFAs碳库的比例以真菌最高,表明真菌对植物残体碳具有最强的同化能力;而残体碳对PLFAs的贡献在革兰氏阳性菌和革兰氏阴性菌之间却差异不大.残体碳含量、PLFAs含量和残体碳占微生物PLFAs碳库的比例均在较小粒级的团聚体中（0.25~1mm和<0.25mm）更高,而细菌/真菌比在较大粒级团聚体（>2mm和1~2mm）中更高,说明较小粒级团聚体已经成为微生物对残体进行同化固定的主要位点.植物残体在土壤中的腐解过程与残体类型、土壤团聚体组成和微生物群落密切相关.     

3种腐熟剂促进玉米秸秆快速腐解特征

为筛选出适宜东北寒冷区快速腐解秸秆的腐熟剂,通过网袋腐解试验明确施入3种秸秆腐熟剂对玉米秸秆生物量及养分释放的影响。结果显示：经过100 d的腐解,玉米秸秆生物量失重率随着时间的延长逐渐增加,玉米秸秆失重率为57.1%-64.1%,其中以施用3号秸秆腐熟剂的玉米秸秆生物量失重率最高,为64.1%。施入不同秸秆腐熟剂后玉米秸秆氮、磷、钾释放率分别为35.1%-57.2%、44.2%-59.6%、77.4%-89.7%,其中以3号腐熟剂的秸秆磷、钾素释放率最高。各处理有机碳矿化率呈相同的趋势,均随时间的延长逐渐增加,取样末期有机碳矿化率在65.3%-69.1%之间,且各处理间差异不明显。综上,以3号秸秆腐熟剂腐解秸秆的效果最好。     

Modelling the impact of thermal adaptation of soil microorganisms and crop system on the dynamics of organic matter in a tropical soil under a climate change scenario

No consensus currently exists about how climate change should affect the status of soil organic matter (SOM) in the tropics. In this study, we analyse the impact of climate change on the underlying mechanisms controlling SOM dynamics in a ferralsol under two contrasting tropical crops: maize (C4 plant) and banana (C3 plant). We model the effect of microbial thermal adaptation on carbon (C) mineralisation at the crop system scale and introduce it in the model STICS, which was previously calibrated for the soil-crop systems tested in this study. Microbial thermal adaptation modelling is based on a reported theory for thermal acclimation of plant and soil respiration. The climate is simulated from 1950 to 2099 for the tropical humid conditions of Guadeloupe (French Antilles), using the ARPEGE model and the IPCC emission scenario A1B. The model predicts increases of 3.4 °C for air temperature and 1100 mm yr⁻¹ for rainfall as a response to an increase of 375 ppm for atmospheric carbon dioxide concentration in the 2090-2099 decade compared with the 1950-1959 decade. The results of the STICS model indicate that the crop affects the response of SOM to climate change by controlling the change in several variables involved in C dynamics: C input, soil temperature and soil moisture. SOM content varies little until 2020, and then it decreases faster for maize than for banana. The decrease is weakened under the hypothesis of thermal adaptation, and this effect is greater for maize (−180 kg C ha⁻¹ yr⁻¹ without adaptation and −140 kg C ha⁻¹ yr⁻¹ with adaptation) than for banana (−60 kg C ha⁻¹ yr⁻¹ and −40 kg C ha⁻¹ yr⁻¹, respectively). The greater SOM loss in maize is mainly due to the negative effect of warming on maize growth decreasing C input from residues. Climate change has a small effect on banana growth, and SOM loss is linked to its effect on C mineralisation. For both crops, annual C mineralisation increases until 2040, and then it decreases continuously. Thermal adaptation reduces the initial increase in mineralisation, but its effect is lower on the final decrease, which is mainly controlled by substrate limitation. No stabilisation in SOM status is attained at the end of the analysed period because C mineralisation is always greater than C input. Model predictions indicate that microbial thermal adaptation modifies, but does not fundamentally change the temporal pattern of SOM dynamics. The vegetation type (C3 or C4) plays a major role in SOM dynamics in this tropical soil because of the different impact of climate change on crop growth and then on C inputs.     

A comparative study of modified and unmodified maize tassels for removal of selected trace metals in contaminated water

Powdered maize tassels were studied and found to exhibit metal sorption properties due to the availability of functional groups. The tassels have a high amount of soluble organic substances that can dissolve in aqueous media, contributing to secondary pollution during a water treatment process. A chelating agent was chemically attached on the maize tassels with a view to increase the sorption capacity, minimize leaching, and enhance the tassels’ stability. Thermogravimetric analysis confirmed that modification improved their thermal stability to withstand temperatures above 600°C as well as reduced the “secondary pollution”. The modified sorbent was employed for the sorption of lead, copper, and cadmium ions in both the model solutions and the real samples. The contact time and pH were optimized after which Langmuir and Freundlich isotherms were applied to the data. The sorption capacities for Cu²⁺, Cd²⁺, and Pb²⁺ improved from 3.4, 0.8, and 1.7?g?kg^?1, respectively, to 6.3, 2.6, and 2.6?g?kg^?1 in the same order. The sorbent was shown to remove up to 95% of the metals in less than 10 min. This study has a potential application for the remediation of polluted waters.     

苗期玉米、大豆在土壤-植物系统N2O排放中的贡献

为区分植物在土壤-植物系统N₂O排放中的贡献,用封闭式箱法对在温室内砂培和土培的玉米、大豆幼苗及砂、土、砂-植物系统、土壤-植物系统的N2O排放进行了测定,同时对植物N₂O排放与植物叶片中的硝酸还原酶(NR)活性及NO₃^--N、NO₂^--N含量的关系进行了分析.结果表明:在53d的观测期内,玉米、大豆幼苗本身均可排放N₂O,且在土壤(砂)-植物系统的N₂O排放中占有很大份额(79.18%～100%);植物N₂O的排放与植物叶片的硝酸还原酶活性和NO₃^--N、NO₂^--N的含量显著正相关(R²≥0.97,n=6).