生物质炭施用及老化对石灰性紫色土中磺胺类抗生素迁移特征的影响

以长江上游低山丘陵区广泛分布的石灰性紫色土旱地的耕作层土壤为对象,采用室内批量平衡吸附试验和填装土柱穿透试验,研究了施用1%生物质炭及3年老化作用对2种磺胺类抗生素(磺胺嘧啶和磺胺二甲基嘧啶)吸附和迁移特征的影响。结果表明,Freundlich方程能更好地拟合抗生素在土壤中的等温吸附曲线,施用生物质炭提高了土壤对抗生素的吸附能力,吸附常数KF值依次为:老化1%施炭土新鲜1%施炭土对照土;土柱出流液的磺胺嘧啶和磺胺二甲基嘧啶相对浓度峰值均表现为:老化1%施炭土新鲜1%施炭土对照土,说明生物质炭的添加能有效减少控制紫色土中抗生素的淋失迁移,以对磺胺二甲基嘧啶的阻控效果较好;生物质炭老化3 a后土壤对抗生素的吸附作用与阻控效果均有所提高,主要归因于土壤pH的提高。     

磺胺嘧啶在原状土柱中的运移特征及模拟

以磺胺嘧啶(Sulfadiazine,SDZ)为研究对象,通过室内原状土柱(0~15 cm,土柱Ⅰ和15~30 cm,土柱Ⅱ)出流试验探讨了其在不同剖面深度处的迁移特征,运用Hydrus-1D软件对试验结果进行模拟,并对不同流速下磺胺嘧啶在0~200 cm土壤中的迁移行为做了预测。结果表明:SDZ在原状土柱Ⅱ中的穿透曲线相较于原状土柱Ⅰ的发生左移,即较深层土壤中,SDZ的迁移速度更快,这主要是受土壤理化性质,如有机质、阳离子交换量和p H等的影响;两区模型(TRM)模拟的R~20.91,均方根误差RMSE0.061,不动水区域f0.154,其模拟效果优于单点模型(OSM)和两点模型(TSM),表明土壤的不可动区域是吸附SDZ的重要部分。预测结果显示:同一流速时,SDZ浓度峰值随着土壤剖面深度增加而减小,出流时间逐渐增大;同一深度处,当水流速度从0.017 cm min~(-1)增加到0.030 cm min~(-1)再到0.100 cm min~(-1)时,磺胺嘧啶在土壤中的迁移速度不断加快,出流浓度也越来越高,当流速为0.100 cm min~(-1)时,SDZ可快速穿过土层进入地下水,其穿透曲线不再对称,出现拖尾现象。     

重金属铅镉胁迫对芋生长发育和产量的影响

采用盆栽试验研究了0(对照),500、1 000、1 500、2 000 mg·kg~(-1)和2 500 mg·kg~(-1)6个浓度的铅(Pb)与0(对照)、0.5、1.0、1.5、2.0 mg·kg~(-1)和2.5 mg·kg~(-1)6个浓度的镉(Cd)溶液分别处理土壤对芋生长发育和产量的影响。结果表明,Pb胁迫抑制芋植株的生长,株高最大低于对照25.3%,对芋叶长、叶宽的影响不显著;而Cd浓度在1.0 mg·kg~(-1)以上显著促进了植株的生长,株高最大高于对照42.1%,最大叶长高于对照60.1%,最大叶宽高于对照60.9%。在1 000 mg·kg~(-1)和1 500 mg·kg~(-1)Pb胁迫下,叶绿素含量显著高于对照,浓度大于1.0 mg·kg~(-1)时Cd胁迫显著高于对照;Pb胁迫MDA含量同比对照显著增加,最大增加了60.8%,Cd胁迫仅在1.0mg·kg~(-1)显著高于对照45.4%。Pb胁迫可溶性糖含量先升后降,1 000 mg·kg~(-1)时显著高于对照40.6%,Cd胁迫时呈上升趋势,最大高于对照33.5%;Pb胁迫可溶性蛋白呈上升趋势,最大高于对照144.0%,Cd胁迫时先上升后下降,1.5 mg·kg~(-1)时显著高于对照37.0%;Pb、Cd胁迫均使SOD活性下降,最大下降幅度分别为37.8%和60.0%,使POD和CAT活性增强,POD最大增强幅度分别为119%和78.7%,CAT最大增强幅度分别为298.5%和65.5%。Pb或Cd胁迫均导致芋产量明显下降,最大下降分别为53.6%和56.5%。     

磺胺嘧啶在黑土及其不同粒径组分中的吸附行为研究

采用批平衡吸附试验法,研究了磺胺嘧啶在黑土及其不同粒径中的吸附行为。结果表明,磺胺嘧啶的吸附不同程度地偏离线性模型,但均可用Freundlich模型和Langmuir模型进行良好地线性拟合。黑土（〈0.2mm）及其不同粒径（粘粒：〈0.002mm、粉粒：0.002~0.02mm、砂粒：0.02~0.2mm）的Freundlich容量因子Kf值分别为29.6、53.1、32.9L.kg-1和21.6L.kg-1,说明磺胺嘧啶在黑土及其不同粒径中的吸附行为存在差异。将吸附参数Kf进行碳标化处理后,Koc值除粉粒外,其他基本一致。随着溶液pH的持续增加（1.0~10.0）,黑土及其不同粒径中的磺胺嘧啶的吸附参数lgKf呈现先急剧降低然后稍微回升的趋势,由此推测,阳离子交换作用可能是磺胺嘧啶土壤吸附的重要机制。过氧化氢处理去除土壤有机质后,黑土的Kd值从1.92L.kg-1降为1.22L.kg-1,磺胺嘧啶的吸附量由16.5mg.kg-1降低到11.2mg.kg-1,说明有机质含量也是影响磺胺嘧啶吸附行为的重要因素。     

镉胁迫对黄麻光合作用及镉积累的影响

为揭示镉(Cd)胁迫下黄麻的光合耐性及其对Cd的富集特征,通过土壤盆栽试验分析了Cd胁迫下黄麻的生长、光合色素、气体交换参数及对Cd富集能力的变化。结果表明,当Cd浓度≤10 mg·kg~(-1)时,黄麻根长、株高和各器官生物量降幅较小;而当Cd浓度≥20 mg·kg~(-1)时,根长、株高和各器官生物量降幅进一步增大。随着Cd浓度的升高,黄麻叶片光合色素含量显著降低,但却能维持较高的Chla/b值,这可能有助于黄麻对Cd的耐性。Cd胁迫使净光合速率(Pn)、气孔导度(Gs)和蒸腾速率(Tr)显著降低,但胞间二氧化碳浓度(Ci)随Cd浓度的升高而逐渐增大,表明黄麻光合速率的下降是由非气孔限制因素引起的。随着Cd浓度的升高,黄麻各器官Cd含量和累积量逐渐增大,在浓为100 mg·kg~(-1)Cd处理下,地上部和地下部Cd含量均达到最大值,分别为232.46 mg·kg~(-1)和186.98 mg·kg~(-1)。Cd胁迫下,黄麻地上部和地下部富集系数均大于1,各处理迁移系数在0.85~1.65之间,表明黄麻对Cd有较强的富集和转运能力。Cd浓度为5~10 mg·kg~(-1)时,Cd提取率超过1.9%。因此,黄麻是一种潜在的修复轻、中度土壤Cd污染的植物材料。本研究结果为挖掘新的植物修复材料提供了理论依据。     

闽西南崩岗土壤重金属含量、分布、来源及生态风险

选取福建省长汀县黄泥坑崩岗群内2处典型崩岗及附近一无崩岗山坡(对照区),采样并测定了63份0~20 cm土壤样品Cu、Zn、Ni、Pb、Cr、As、Cd含量,运用相关分析与主成分分析进行重金属来源辨识,并应用Hankanson潜在生态风险指数法,以福建省背景值和国家二级标准作为参比,对研究区重金属进行潜在生态风险评价。结果表明:研究区土壤重金属含量从高到低的顺序依次为Zn(105.56 mg·kg~(-1))Pb(67.21 mg·kg~(-1))As(61.47 mg·kg~(-1))Cu(22.33 mg·kg~(-1))Cr(17.12 mg·kg~(-1))Ni(5.24 mg·kg~(-1))Cd(0.80 mg·kg~(-1)),Pb、Cd含量表现为崩岗区对照区,Cu、Zn、Ni、Cr、As、Cd含量与之相反。1号崩岗Zn、Pb、As和Cd平均值分别是福建省背景值的1.12倍、2.82倍、8.68倍和13.33倍,2号崩岗这4种元素平均值分别是背景值的1.11倍、1.36倍、11.22倍和16.67倍,对照区该4种元素平均值分别是背景值的1.58倍、1.60倍、5.14倍和14.44倍;与国家土壤环境质量二级标准比较得出,崩岗区和对照区As平均值分别超标1.92倍和2.70倍,Cd平均值分别超标2.31倍和2.60倍。从集水坡面到沟道末端,崩岗区Pb、Zn、Cd含量呈增加趋势,Cu、Cr含量基本维持稳定,Ni含量有所降低;从坡面上部到下部,对照区Cu、Zn、Ni、Cr、Cd含量呈增加趋势,Pb含量略有降低;As含量在研究区的分布无明显变化。Cu、Ni、Cr主要来源为成土母质,Zn主要来源于禽畜养殖,Cd、As的主要来源包基岩风化稀土开采,Pb主要来源于基岩矿化、煤炭燃烧及汽车尾气排放等复合污染源。以福建省背景值为参比时,Cd潜在生态风险系数达到"极强风险",As为"较强风险",其余均为"轻微风险";以国家二级标准为参比时,Cd属"较强风险",其余均为"轻微风险"。潜在生态风险指数(Ri)表现为2号崩岗对照区1号崩岗。研究区Cd、As污染已较为严重,应采取相应的安全防范措施。     

Cu/Pb/Zn/Cd在石英砂中的迁移实验及模拟

通过稳定流混合置换实验,研究了孔隙水流速和pH变化对Cu/Pb/Zn/Cd在石英砂中迁移行为的影响,获得了示踪剂Br-和Cu/Pb/Zn/Cd的穿透曲线(BTCs);并通过室内批量平衡实验获得吸附系数,进而计算出阻滞因子Rd。基于这些实验结果,借助CXTFIT2.1软件,用平衡CDE模型拟合了Br-的BTCs,得到了弥散系数D;在此基础上应用CDE非平衡模型拟合Cu/Pb/Zn/Cd在不同流速和pH条件下的BTCs,并预测了平行实验和不同埋深处Cu/Pb/Zn/Cd浓度的动态变化。结果表明,Cu/Pb/Zn/Cd的迁移能力随流速的增大而增强,而随pH的增大而降低;化学非平衡的两点模型能较好地模拟本文实验条件下Cu/Pb/Zn/Cd的迁移过程。     

磺胺嘧啶在土壤及土壤组分中的吸附/解吸动力学

抗生素在土壤中的吸附/解吸及迁移过程受其理化性质的强烈影响,其中土壤中的矿物成分,如高岭石、蒙脱石及腐殖酸等是重要控制因素。本文主要研究了磺胺嘧啶在土壤、高岭石、蒙脱石和腐殖酸中的吸附/解吸动力学过程,并对反应前后的高岭石、蒙脱石和腐殖酸进行傅里叶红外光谱(Fourier transform infrared, FTIR)表征,探讨其可能的吸附机理。结果表明:磺胺嘧啶的吸附(解吸)动力学过程,可以分为快速吸附(解吸)、吸附解吸动态平衡和吸附(解吸)平衡3个阶段;磺胺嘧啶在土壤及其3种组分中的吸附(解吸)均可在24 h内达到平衡,其浓度高低会导致土壤及其组分的吸附差异,不同土壤组分中的官能团含量、带电性质及氢键是造成吸附差异的主要原因;分别用伪一级动力学模型、伪二级动力学模型和Elovich模型对其吸附过程进行拟合,其动力学吸附过程更符合伪二级动力学模型,R20.99,主要受控于物理化学吸附;FTIR图谱表明磺胺嘧啶与高岭石以物理吸附为主,并有少量氢键作用,与蒙脱石之间主要以氢键作用完成吸附,而在腐殖酸中存在表面络合和π–π共轭作用。     

河北板蓝根产地土壤-植物中镉铅汞砷含量特征及其污染评价

采用野外调查和室内分析相结合的方法,研究了河北省安国市和蔚县板蓝根产地土壤-植物中Cd、Pb、Hg、As含量特征及其在菘蓝中的累积特性,并对板蓝根产地土壤和草药中Cd、Pb、Hg、As污染状况进行了评价,为该地区安全、合理地发展中草药生产提供数据支撑和科学依据。结果表明,安国市和蔚县板蓝根产地土壤中重金属Cd、Pb、Hg、As含量差异不大,土壤重金属含量的变异系数在11.70%~97.65%。以《土壤环境质量标准》(GB 15618—1995)一级标准值进行评价,综合污染指数评价结果显示45%板蓝根种植区土壤Cd、Pb、Hg、As污染等级为警戒限,其他处于清洁水平;而以《土壤环境质量标准》二级标准值进行评价,种植区单项污染指数及综合污染指数结果均0.7,土壤环境清洁。此外,菘蓝地上部(大青叶)Cd、Pb、Hg、As平均含量分别为0.22 mg·kg~(-1)、0.89 mg·kg~(-1)、0.04 mg·kg~(-1)、0.25 mg·kg~(-1),对重金属的富集能力表现为CdHgPbAs;菘蓝地下部(板蓝根)Cd、Pb、Hg、As含量均值分别为0.14 mg·kg~(-1)、0.57 mg·kg~(-1)、0.04 mg·kg~(-1)、0.26 mg·kg~(-1),对重金属的富集能力表现为CdHgAsPb。所有菘蓝样品中Pb、Hg、As含量均未超出《药用植物及制剂进口绿色行业标准》(WM2—2001),大青叶9.09%样品中Cd超标,且Cd平均污染指数0.7,属警戒限污染等级。因此,在中药材GAP(良好的农业规范)产地环境质量评价时,除板蓝根产地土壤完全符合土壤环境质量二级标准外,也不应忽视板蓝根和大青叶吸收和累积重金属的自身特性。     

含Pb、Cd细颗粒物暴露对水稻、马铃薯早期生长的影响

大气含重金属细颗粒物对陆生植物的早期生长有负面影响。通过搭建合理的暴露场景,在植物早期生长阶段,模拟不同程度大气污染条件,评价含Pb、Cd重金属细颗粒物对水稻、马铃薯2种受试植物出苗、幼苗生长和鲜重(陆上茎叶和地下块茎两部分)等生物量的影响。结果显示,暴露处理组人工土壤Cd、Pb元素浓度在试验结束时均有增加,其中Cd元素浓度比背景值增加了约8.8倍,Pb元素浓度增加相比背景值不明显。水稻陆上茎叶部分对Cd、Pb的富集量分别为0.002 0 mg·kg~(-1)和0.054 mg·kg~(~(-1));马铃薯地下块茎部分对Cd、Pb的富集量分别为0.185 0 mg·kg~(-1)和0.074 mg·kg~(-1)。暴露处理后对水稻的各生物量终点抑制效应不明显,而对马铃薯地下块茎鲜重的抑制率达到27%。由此可见,在模拟暴露条件下,人工土壤Cd污染元素浓度变化较大,马铃薯地下块茎对Cd元素富集效应明显。与空白对照组相比,暴露处理导致的Pb-Cd重金属复合污染对于马铃薯地下块茎生物量有显著的抑制效应和胁迫效应。同时,水稻陆上部分对于暴露的污染物及设定浓度表现出较好的适应性和低敏感性。     

Abundance of Frankia from Gymnostoma spp. in the rhizosphere of Alphitonia neocaledonica, a non-nodulated Rhamnaceae endemicto New Caledonia

The capacity of different soils of New Caledonia to induce nodulation in Gymnostoma poissonianum was studied. The soils were sampled under five Gymnostoma species, Alphitonia neocaledonica (a non-nodulated endemic Rhamnaceae) and Pinus caribea (an introduced species) growing in various ecological conditions. Using G. poissonianum as trap-host, we observed a higher abundance of Frankia from Gymnostoma spp. in the rhizosphere of A. neocaledonica as compared with bare soils and P. caribea rhizosphere. The nodulating capacity of A. neocaledonica rhizosphere was almost similar to that of the five Gymnostoma species (symbiotic host) studied in the same stations. In comparison, bare soils or rhizosphere of P. caribea had poor nodulating capacities. We isolated fourteen Frankia strains from nodules of G. poissonianum after baiting with the rhizospheric soils of five Gymnostoma and A. neocaledonica. Using the PCR/RFLP method, we confirmed the similarity with those already described. Frankia was abundant in the rhizosphere of A. neocaledonica in all the sites studied. One explanation could be a positive tropism of Frankia towards species belonging to families having nodulated species, which is the case of A. neocaledonica endemic in New Caledonia. We can suppose that the non-nodulated plants belonging to these families can excrete some chemical substances able to attract Frankia and to induce its proliferation.     

Determination of kC and kNin situ for calibration of the chloroform fumigation-incubation method

¹⁴C-labelled glucose and ¹⁵N-labelled KNO₃ were added to soil and the microbial biomass during 42 days' incubation was estimated using the chloroform fumigation-incubation method (CFIM). By day 1, most of the glucose (1577 μgCg^?1 soil) was metabolized and 110 μg NO^?₃-Ng^?1 soil were immobilized. In situ values for the proportions of biomass C (k_C) and biomass N (k_N) mineralized during the 10 days after CHCl₃ fumigation were determined on the basis that the immobilized labelled C and N remaining in the soil at this time were present as living microbial cells and their associated metabolites. The tracer data indicated that biomass C could be calculated by applying a k_c value of 0.41 to the CO₂-C evolved from the fumigated sample without subtraction of an unfumigated “control”. Biomass N was estimated from the net NH₄^?-N accumulation during the fumigation-incubation. The problem of reimmobilization of NH⁺₄-N where organisms of wide C:N ratio occur was overcome by adjusting the value of k_N according to the ratio of CO₂-C evolved: net NH₄⁺-N accumulated during the fumigation-incubation (C_F:N_F).A C_F:N_F ratio of 6:1 resulted in a k_N of 0.30 whereas a ratio of 13:1 indicated a k_N of 0.20.     

Comparison of volatile generation in serine/threonine/glutamine-ribose/glucose/fructose model systems

Thermal generation of volatiles in nine model reactions was studied and compared. Each of the model systems contained one amino acid and one monosaccharide. The amino acid was serine, threonine, or glutamine, and the monosaccharide was ribose, glucose, or fructose. More unsubstituted pyrazine was generated in serine-sugar systems than threonine-sugar systems. The formation of several furfuryl-substituted pyrazines and pyrroles was observed in some of the studied systems. Total pyrazines were generated more in glutamine-containing systems than in serine- and threonine-containing systems, and the reverse was true for generation of furfuryl-substituted compounds. Acetylpyrazine was generated in serine/threonine/glutamine-glucose and serine/glutamine-fructose systems.     

Incorporation studies of NH+4 during incubation of organic residues by l5N-CPMAS-NMR-spectroscopy

This study focuses on the processes occurring during incorporation of inorganic nitrogen into humic substances. Therefore rye grass, wheat straw, beech saw dust, sulphonated lignin and organosolve lignin were incubated together with highly ¹⁵N-enriched ammonium sulphate in the laboratory for 600 days. Samples from the incubates were periodically analysed for weight loss, and carbon and nitrogen contents. The samples were also analysed by solid-state ¹³C- and ¹⁵N-CPMAS-NMR-spectroscopy to follow the turnover of the materials during incubation. Most of the detectable N-signals was assigned to amide - peptide structures. The remaining intensities could be ascribed to free and alkylated amino groups, and those on the low field side of the broad amide-peptide signal to indole, pyrrole and nucleotide derivatives. Abiotic reactions of ammonia with suitable precursors and the formation of pyridine, pyrazine or phenyloxazone derivatives were not observed. Signals from ammonia and nitrate occurred only at the end of the incubation.     

Diffusion of NH+4 and NO−3 mineralized from organic N in soil

The mineralization of native soil organic matter and the simultaneous diffusion of zero NH⁺₄ and NO^?₃ to a solution sink of zero N concentration was analysed experimentally and theoretically for a fine sandy loam soil. Experimentally, the NH₄ and NO₃ ions produced in an incubated unsaturated soil column were allowed to diffuse through a sintered glass plate into a stirred solution sink. The distribution of NH⁺₄ and NO^?₃ in the soil column was measured after various incubation times. The rate of ammonification was measured directly during incubation and the rate of nitrification modelled from nitrifier growth kinetics. A Freundlich equation was used to describe the equilibrium between soluble and exchangeable NH⁺₄ in the soil. Terms for the microbial transformation of N and the adsorption-desorption of NH⁺₄ were combined with diffusion equations which were solved numerically using finite difference methods. The model constructed was used to predict the NH⁺₄ and NO^?₃ con-centration distributions in the soil column, and good agreement was obtained between the experimental and predicted concentration profiles. The use of the model for predicting the diffusive flux of mineral N to the outer surfaces of soil peds, where it is vulnerable to leaching, was demonstrated.     

Chemical and colloidal stability of sols in the Al2O3-Fe2O3-SiO2-H2O system: their role in podzolization

Concentrations of dialysable silica in equilibrium with Al₂O₃-SiO₂-H₂O sols at pH 4.5–5.0 confirm the formation of a poorly ordered non-dialysable proto-imogolite species with an Al : Si ratio near 2, close to that of imogolite. Sols with Al : Si>2 give nearly constant levels of free silica in solution in the range 2–6 μg/cm³, indicating equilibrium between proto-imogolite and aluminium hydroxide species. These findings indicate that imogolite-like precipitates in acid soils will buffer silica in solution to within this range during leaching episodes. Imogolite is more stable than a previous estimate suggested, and a revised value for its free energy of formation is proposed: ΔG⁰_f(298.15) = -2929.7 kJ/mol. In Fe₂O₃-SiO₂-H₂O sols, the Fe : Si ratio of the non-dialysable species varies smoothly from 11 to 3 as free silica in solution ranges from 4 to 35 μg/cm³. Such sols are much less colloidally stable than hydroxyaluminium silicate sols, but mixed Al₂O₃—Fe₂O₃—SiO₂—H₂O sols are almost as stable as iron-free sols up to a Fe : Al ratio of 1.5. Thus migration of Al and Fe as mixed hydroxide sols can account for the almost constant ratio of Al to Fe with depth in oxalate extracts from Bs horizons of podzols.     

不同铵硝比例对杭白菊次生代谢及抗病性的影响

【目的】 氮素形态与寄主营养和病害严重度的关系一直是人们关注的热点,氮素营养对植物次生代谢产物的影响也多有研究。斑枯病为杭白菊常见病害,黄酮和酚酸类物质是杭白菊主要的资源性化学成分。针对杭白菊生产中存在的问题,本文对不同铵硝比例处理下杭白菊的次生代谢及斑枯病发病情况进行调查和研究,以期为杭白菊生产过程中的氮素配施、 病害防治和次生代谢调控提供一定的技术借鉴。【方法】 采用盆栽试验,在总施氮水平相同的前提下,设置5个NH+4和NO-3比例,采用随机区组设计,管理措施一致,4次重复。采取对角线定点定株定期调查杭白菊斑枯病发病情况,采用描叶法和LI-3000C叶面积仪来确定植株病害状况,统计病情指数和病害发生率;测定苯丙氨酸解氨酶(PAL)、 木质素、 纤维素、 可溶性总糖、 可溶性蛋白、 超氧阴离子(O-2)、 丙二醛(MDA)等相关生理指标,超氧化物歧化酶(SOD)和过氧化物酶(POD)等抗氧化酶;测定不同处理下杭白菊花中次生代谢产物绿原酸、 木犀草苷、 3,5-O-双咖啡酰基奎宁酸以及根、 茎、 叶等不同部位总黄酮含量。对相关生理指标与发病率和病情指数进行相关性分析。【结果】 当铵硝比为25:75时木质素、 纤维素、 可溶性总糖、 POD、 苯丙氨酸和O-2含量达到最大值,MDA含量和SOD活性相对较低;杭白菊根、 茎、 叶及花中总黄酮的含量在铵硝比为25:75和0:100时均表现出较高的含量,绿原酸、 3,5-O-双咖啡酰基奎宁酸两者的含量在铵硝比为25:75时达到最大值,分别为0.67%和1.84%。随着硝态氮比例的增加杭白菊斑枯病的发病率和病情指数均有所下降。相关性分析显示木质素、 可溶性总糖、 PAL活性、 POD活性、 超氧阴离子、 绿原酸、 3,5-O-双咖啡酰基奎宁酸、 花中总黄酮的含量与杭白菊斑枯病的发病率和病情指数呈负相关,且达到极显著水平;SOD活性、 MDA含量与杭白菊斑枯病的发病率和病情指数呈正相关,且均达到显著水平。【结论】 杭白菊斑枯病的发病率和病情指数与相关生理指标和次生代谢密切相关,不同铵硝比例对药用菊花次生代谢产物及斑枯病的发生有一定的影响,当铵硝比为25:75时菊花斑枯病的发病率最低。     

Rhizobium inoculation of Calopogonium caeruleum

The shade-tolerant cover legume Calopogonium caeruleum is promiscuous in its nodulating habits. In sand culture, symbiotic effectiveness of the strains tested was variable; 6 strains of rhizobia markedly improved shoot yields and 20 increased shoot N content. In pot experiments using cultivated and non-cultivated soils, inoculation gave no significant increase in shoot yields. When grown under rubber in plantation conditions at four localities, shoot dry matter yields, N content and nodulation also were not different from uninoculated plants when sampled for up to 2 yr after planting. This occurred despite the low numbers (< 10 g^?1 soil) of native rhizobia at some sites and an appreciable establishment (> 70% recovery in nodules) by the inoculant strains.     

Assessment of N2O, NOx and NH3 emissions from a typical rural catchment in Eastern China

To evaluate the atmospheric load of reactive gaseous nitrogen in the fast-developing Eastern China region, we compiled inventories of nitrous oxide (N₂O), nitrogen oxide (NO_x) and ammonia (NH₃) emissions from a typical rural catchment in Jiangsu province, China, situated at the lower reach of the Yangtze River. We considered emissions from synthetic N fertilizer, human and livestock excreta, decomposition of crop residue returned to cropland and residue burning, soil background and household energy consumption. The results showed that, for the 45.5 km² catchment, the annual reactive gaseous emission was 279 ton N, of which 7% was N₂O, 16% was NO_x and 77% was NH₃. Synthetic N fertilizer application was the dominant source of N₂O and NH₃ emissions and crop residue burning was the dominant source of NO_x emission. Sixty-seven percent of the total reactive gaseous N was emitted from croplands, but on a per unit area basis, NO_x and NH₃ emissions in residential areas were higher than in croplands, probably as a result of household crop residue burning and extensive human and livestock excreta management systems. Emission per capita was estimated to be 18.2 kg N year⁻¹ in the rural catchment, and emission per unit area was 56.9 kg N ha⁻¹year⁻¹ for NH₃ + NO_x, which supports the observed high atmospheric N deposition in the catchment. Apparently, efficient use of N fertilizer and biological utilization of crop straw are important measures to reduce reactive gases emissions in this rural catchment.     

Blocking the release of potassium from clay interlayers by small concentrations of NH4+ and Cs+

To understand the process and the kinetics of potassium release from the clay interlayer in natural and arable soils in more detail, I tested the hypotheses that large, monovalent cations, especially NH₄⁺ and Cs⁺, can reduce the release rates of K⁺ which is exchanged by Ca²⁺, even if these monovalent cations are present in concentrations of only a few μm . Percolation experiments were carried out with different illitic soil materials, some containing vermiculite, with 5 m m CaCl₂ at pH 5.8 and 20°C, in some cases for over 7000 h. NH₄⁺ and Cs⁺ both caused a large decrease in the rate at which K⁺ was released, Cs⁺ especially. Suppression began at 5 μm NH₄⁺ Blocking by 20 μm NH₄⁺ was easily reversible: the release rates readily increased when NH₄⁺ was omitted from the exchange solution. Blocking by 2 μm Cs⁺ was equal to approximately 90% of that at 10 μm Cs^+. Larger concentrations of Cs⁺ than 10 μm did not further reduce release but rather caused a slight increase, probably because of enhanced exchange of K⁺ by Cs⁺ without exfoliation of the interlayer space. Blocking by Cs⁺ was not reversible within > 7000 h of percolation by 5 m m CaCl₂. The blocking effect was reproduced in several different soil materials using 10 μm Cs⁺ but was most pronounced in vermiculite-rich samples. As NH₄⁺ is present in most arable soils, at least in concentrations of a few μm , I conclude that the observed effects are of significance in the K dynamics processes in soils, for example near the roots of plants. Further, very small concentrations of Cs⁺ in exchange solutions containing a large background of Ca²⁺ appear to be useful for suppressing K⁺ release from the interlayer in laboratory studies, probably without significantly altering the exchange at outer mineral surfaces.