Relationships between volatile organic compounds with an emphasis on terpene compounds and genetic matrix in inoculated and non-inoculated winter wheat cultivars

In the present study, we focus on the analysis of the volatile organic compound (VOC) contents in the grain of a representative set of winter wheat cultivars grown in Central Europe. The cultivars were grown in control conditions or were inoculated with the fungus Fusarium culmorum. In the analysed samples, hydrocarbons, alcohols, aldehydes and ketones, aromatics, terpenes and others were found. Among them, results for terpenes seem particularly important. The discriminant analysis allowed complete separation of the quality groups of wheat based on VOCs. Simultaneously, a genetic matrix was created based on the genetic distance between the wheat cultivars and the Mantel test was used to compare it with the VOC matrix. The analysis revealed relationships between the genetic matrix and the overall VOCs, as well as terpenes. The obtained results indicate a significant relationship between microorganisms that exist in the environment, genetic features of plants and VOCs formed in the grain.     

Magnetic particles precipitated onto wheat husk for removal of methyl blue from aqueous solution

Magnetic particles prepared via co-precipitation and impregnated onto wheat husk (MN-WH) were used for the removal of methyl blue (MB) from aqueous solution. Experiments were conducted in a batch mode for optimization regarding pH, contact time, adsorbent dose, initial dye concentrations, and temperature. Maximum adsorption (98%) was achieved at pH 5. The adsorption data were fitted into pseudo-first, pseudo-second, intraparticle diffusion, and Elovich equation revealing that adsorption followed pseudo-second-order kinetics. The four most common isotherm models, i.e. the Langmuir, Freundlich, Tempkin, and Dubinin–Radushkevich (D–R), were used to evaluate the data, with the best fit to a Langmuir isotherm (R² = 0.996), followed by a Freundlich isotherm (R² = 0.995), indicating monolayer adsorption of MB on the surface of MN-WH. Thermodynamic parameters calculated from the Van't Hoff equation revealed that the adsorption is exothermic (ΔHº = ?19.7 kJ mol^?1).     

Persistence of the sulfonylurea herbicide iodosulfuron-methyl in the soil of winter wheat crops

On four winter wheat fields grown on soils of different textures in Belgium, 10?g a.i.?ha^?1 of the sulfonylurea herbicide iodosulfuron-methyl-sodium was applied post-emergence in the spring. A procedure was developed for the analysis in field soils of iodosulfuron-methyl 1 and of its metabolites iodosulfonamide 2 and iodosaccharin 3 with a sensitivity limit of 0.3?µg of equivalents of iodosulfuron-methyl 1 kg^?1 dry soil. GC and GC-MS was used after purification of the soil extracts by repeated TLC, and methylation. The results of the chemical analyses were confirmed by means of bioassays using sugar beet as test plants. On a winter wheat crop grown on sandy loam soil of pH 6.2 at Melle, iodosulfuron-methyl-sodium 1 was applied at the beginning of April. The iodosulfuron-methyl 1 soil half-life in the 0–10?cm surface soil layer was 60 days. At the end of June, the sum of the concentrations of the metabolites 2 and 3 in the 0–10?cm surface soil layer attained a maximum corresponding to 27% of the applied dose. Green manures were sown after the harvest of the wheat at the end of August. No phytotoxicity at all was observed during the growth of the green manures, in spite of the very low residues of iodosulfuron-methyl 1 remaining in soil in September and October. At the mid of November, iodosulfuron-methyl 1 and its metabolites 2 and 3 were no more detected in soil. On three other winter wheat crops grown on clay soils of pH of about 8 at Leke, Gistel and Zevekote, iodosulfuron-methyl-sodium 1 was applied at the beginning of May. The soil half-life of iodosulfuron-methyl 1 in the 0–10?cm surface soil layer was between 30 and 44 days. Since the application and until the mid of November, in all the trials made on sandy loam or clay soils, iodosulfuron-methyl 1 (and its metabolites 2 and 3 in the trial made on sandy loam soil) were never detected in the 10–15 and 15–20?cm surface soil layers, indicating their low mobilities in the field soils.     

湖泊底泥土地利用对土壤中重金属铅、铜形态影响

采用田区试验研究了田间种植冬小麦条件下,底泥土地利用前后土壤中重金属铅、铜的形态演变及小麦各器官中铅、铜的富集。结果表明,随着底泥施用量的增加,土壤中重金属铅、铜的可交换态、碳酸盐结合态、铁锰氧化物结合态、有机结合态、残渣态均有不同程度的增加,本试验所有处理中,可交换态铅的质量分数范围为0.02~0.10 mg·kg-1,碳酸盐结合态铅的质量分数范围为0.04~0.24 mg·kg-1,铁锰氧化物结合态铅质量分数为0.41~1.88 mg·kg-1,有机物结合态铅质量分数范围为1.23~4.92 mg·kg-1,残渣态铅质量分数范围为4.82~23.66 mg·kg-1;各处理与对照相比,可交换态铜质量分数增加了40.00%~200.00%,碳酸盐结合态铜质量分数增加了36.84%~363.16%,铁锰氧化物结合态铜质量分数增加了7.17~45.15%,有机结合态铜质量分数增加了7.98%~62.61%,残渣态铜质量分数增加了0.12%~9.69%,各处理的残渣态铅、铜质量分数均较高。随着底泥用量增加,小麦根系、茎叶、籽粒中铅、铜质量分数均呈增加趋势,植株对重金属铅、铜的富集顺序为根系>茎叶>籽粒,铜的富集系数均大于铅。小麦籽粒产量、茎叶生物量及地上部生物量随着底泥施用量的增加,均出现了先增加后减少的现象,当小麦籽粒产量达到最大值时,籽粒中铅、铜质量分数未超出我国相应标准,依此确定底泥环境安全施用量为3051.29 t·hm-2。     

外源NO对不同冬春性小麦花后光合生理的影响

为利用一氧化氮（NO）调节作用实现小麦（Tritivum aestivum L.）高产优质之目的,本试验在网室盆栽条件下,以冬春性不同的2个小麦品种（弱春性偃展4110和半冬性周麦18）为试验材料,研究了不同浓度外源NO供体——SNP处理对花后小麦光合生理特性及成熟期产量构成因素的影响。结果表明,不同浓度SNP处理对2种小麦旗叶叶面积、RWC、可溶性糖、总叶绿素含量、WUE、千粒质量、穗粒质量等均有不同程度的促进作用;与对照相比,低浓度SNP（0.075～0.15 mmol.L-1）明显降低2种小麦旗叶枯叶/绿叶值（Y/G）,而高浓度（0.30 mmol.L-1）处理则使Y/G值上升。综合分析：本试验条件下,外源NO对半冬性品种周麦18的调控效果优于弱春性品种偃展4110;周麦18以0.30 mmol.L-1SNP处理、偃展4110以0.15mmol.L-1SNP调控对小麦增产较为明显。     

铬胁迫下不同品种小麦萌发和内源激素的变化

采用K2(CrO4)3溶液,设5个浓度,对3种不同抗性的小麦品种(新麦19、矮抗58和豫麦18)进行萌发期胁迫处理,研究了幼苗的发芽势、发芽率、根长、芽长及内源激素含量的变化.结果表明:(1)随着铬浓度的增加,发芽势、发芽率和芽长均基本呈"先升后降"趋势;(2)同一浓度铬处理下,发芽率、发芽势和芽长从大到小的顺序依次为:新麦19、矮抗58、豫麦18,根长从大到小的顺序为:豫麦18、新麦19、矮抗58;(3)150 mg L-1的铬胁迫下,IAA与ABA在小麦幼苗、幼根中含量降低,在籽粒中含量升高,其中新麦19籽粒和根芽中ABA含量均高于其他品种的;(4)不同浓度铬胁迫下,IAA/ABA值在新麦19中最低,变化幅度最小,新麦19表现出较强的抵抗铬胁迫能力.图3表1参20     

Cd胁迫下黄土施用污泥对小麦生长及Cd富集迁移的影响

为了能给污泥资源开发利用开辟新的途径,以黄土为供试土壤,小麦（Triticumaestivum L.）为供试作物。采用盆栽试验研究了泥在不同Cd胁迫黄土中对小麦生长的影响及其对小麦各部位Cd的富集迁移规律。试验设计2个污泥处理水平,每个塑料盆中加入8.0 kg供试土壤或污泥含量为4.0%的供试土壤,土壤中以Cd（NO3）2·4H2O溶液形式加入的Cd质量分数分别为0.5、1.0、2.5、5.0、10.0、25.0、50 mg·kg^-1,对应各处理为TS1-TS7。各胁迫水平均设置3个平行,同时设置对照TS0。结果表明,黄土中低水平的Cd胁迫可促进小麦的生长,且在Cd污染水平5.0 mg·kg^-1时施污泥和未施污泥土壤中小麦生物量均最大,而高水平的Cd胁迫抑制小麦的生长,且Cd胁迫水平越高,抑制作用越强烈;Cd胁迫下施用污泥可促进小麦的生长,尤其是茎叶和籽粒的生长;小麦各部位Cd的含量随土壤Cd处理水平的升高而增加且呈显著正相关（P＜0.05）,各部位最大浓度分别可以达到：45.32、14.41、9.66 mg·kg^-1,且根系＞茎叶＞籽粒,污泥的施用能促进小麦对Cd的吸收;小麦各部位对Cd的富集能力均随着土壤Cd胁迫水平的升高而先增加后减小,污泥的施用在一定程度上提高了小麦对Cd的富集能力,各部位富集系数最大分值分别为1.81、0.93、0.51,但对Cd进入小麦根系后向茎叶和籽粒的迁移影响不显著。     

影响不同农作物镉富集系数的土壤因素

农作物的Cd富集系数（BCF）受多种因素影响.为明确田间条件下不同农作物的Cd富集系数特征差异及土壤性质对其影响,分别在我国水稻、小麦和玉米主产区不同污染程度的地块上作物收获期采集土壤和作物籽粒点对点样品,研究水稻、小麦、夏玉米和春玉米的Cd富集系数特征及土壤性质对不同农作物的Cd富集系数的影响,并通过多元回归方程建立以上农作物Cd富集系数与土壤性质的定量关系.结果表明,在田间土壤中Cd含量范围为0.15~2.66 mg·kg^-1条件下,水稻、小麦、夏玉米和春玉米Cd富集系数的均值分别为0.915、0.155、0.113和0.102,水稻明显高于小麦和玉米,春玉米的Cd富集系数最低.土壤中的Cd含量与小麦、夏玉米和春玉米的BCF呈极显著负相关;土壤有机质（SOM）与小麦、夏玉米BCF之间的关系呈极显著负相关;土壤pH和阳离子交换量（CEC）对作物BCF也有影响.引入土壤Cd含量、pH、SOM、CEC等因素,建立水稻、小麦、夏玉米和春玉米的Cd富集系数预测方程.水稻、小麦、夏玉米和春玉米的BCF预测方程相关系数分别为0.423^*、0.796^**、0.826^**和0.551^**,均达到显著或极显著水平,可以较好地预测不同土壤条件下不同农作物的BCF值.     

黄土高原冬小麦田土壤水分与小麦产量对降水和气温变化响应的模拟研究

明确黄土高原地区降水和气温变化对冬小麦田土壤水分和产量的影响,对探索适应气候变化的冬小麦田间管理措施具有重要的现实意义。论文在验证EPIC模型对冬小麦田土壤水分模拟精度的基础上,以历史气象数据为基础,设置TR1、TR2和TR3三个气候情景,采用作物模型模拟的方法,研究黄土高原冬小麦田土壤水分和冬小麦产量对降水和气温变化的响应。结果显示：1）1961—2010年黄土高原降水呈降低趋势,其年际间变化幅度和频率均有所增加。与1961—1970年相比,洛川、长武、运城和延安的年均降水量在2001—2010年间分别降低了18.1%、13.6%、18.8%和24.9%,其变差系数分别增加了0.029、0.087、0.02和0.057。1961—2010年黄土高原气温呈波动性增加趋势,其中日最低气温增加幅度大于日最高气温增加幅度。与1961—1970年相比,日最高气温在2001—2010年间增加了0.30~0.84 ℃,而日最低气温增加了1.00~1.55 ℃。2）EPIC模型能够较好地模拟黄土高原冬小麦田土壤水分动态变化规律,0~2.0 m土层土壤湿度观测值与模拟值间的相对均方根误差RRMSE值为6.0%~14.0%,R²和模型效率ME值分别为0.824和0.815。3）黄土高原地区降水的减少和最高气温的增加均不利于冬小麦生产,而最低气温的提高对冬小麦生产较为有利。洛川、长武、运城和延安冬小麦产量因年降水量的降低而分别减产了8.5%、7.6%、11.7%和12.3%;因日最高气温的升高分别减产了6.4%、6.8%、7.2%和-3.0%;因日最低气温的提高而分别增加了8.8%、10.2%、1.5%和12.0%。因此,为适应降水减少和日最低气温升高的趋势,黄土高原冬小麦生产区应适当调整冬小麦播期,研究并推广保水节水技术措施,充分利用气候变化对冬小麦生产的有利因素,克服不利因素,确保冬小麦的可持续生产。     

天津滨海新区秋冬季大气污染特征分析

为了解天津滨海新区大气污染物浓度水平和污染来源,2009年9月1日~2010年2月28日对NOx、CO、SO2、O3、PM2.5、PM10进行了连续在线观测,并同步观测了气象要素.结果表明,秋冬季上述污染物最高日均值(秋冬平均值±标准差,O3为日小时均值最大值)分别达到300.7(65.4±52.9)×10-9、7.278(1.324±1.169)×10-6、53(13±12)×10-9、95(28±21)×10-9(体积分数)和287.4(62.3±53.6)μg/m3、1421.4(161.9±136) μg/m3. NOx和SO2秋季低于冬季,O3和PM10反之. CO和PM10相对国家二级标准超标率为2%和38%,PM2.5相对WHO标准(75μg/m3)超标率为31%.季节统计日变化显示CO和NOx为早晚双峰型,SO2为中午的单峰型,O3为午后单峰型,且秋季日变化振幅远大于冬季, PM10为早晚双峰型,但冬季比秋季晚出峰2~3h.除冬季PM10,大气污染物浓度49%~74%的逐日变化由气象要素影响.滨海新区大气污染受局地排放和外源输送共同影响,西南方向气流易造成污染物积累,其次是东北方向,而东和东南气流最有利于污染物扩散;各污染物具体表现为NOx主要受局地源控制;SO2主要受外来输送影响;CO和PM2.5同时受本地源和外来源的共同影响;PM10秋季表现为本地源污染,而冬季为本地源和外来源的共同影响.