热解温度对玉米芯生物炭碳结构、灰分与吸附四环素的影响

生物炭灰分和碳结构在抗生素吸附过程中的影响尚不明确。本文以玉米芯为原料,在300~800 ℃下热解制备生物炭（CBCs）及除灰分生物炭（CBCs_AW）,研究热解温度对生物炭灰分和碳结构的影响,探究灰分和碳形态与四环素（TC）吸附行为之间的关系。结果表明,随着热解温度升高,生物炭的碳结构由未完全碳化有机质（300 ℃）逐渐转化为石墨碳结构（800 ℃）,吸附实验结果显示CBC800_AW的吸附量最大,证实石墨碳结构是促进TC吸附量增加的重要因素。CBCs_AW对TC吸附量高于CBCs,说明灰分对TC吸附有一定抑制作用。分析TC吸附性能与生物炭理化性质的相关性,结果显示吸附量与生物炭比表面积、孔体积、芳香性和石墨化程度相关性较高,推测TC的主要吸附机理为孔隙填充作用和π-π电子供体-受体相互作用。研究结果可为生物质资源化利用和抗生素污染修复提供科学依据。     

NaHCO3前处理对生物炭性质及其磷吸附能力的影响

为探究NaHCO₃前处理对不同种类生物炭性质及其磷吸附能力的影响,借助元素分析、光电子能谱、孔径分析、扫描电镜等手段对比处理前后秸秆、壳核及其他3类生物炭表面特性和孔结构的差异,基于吸附等温线和Freundlich与Dubinin-Radushkevich模型拟合,探讨生物炭性质控制磷吸附的机理。结果表明：NaHCO₃前处理总体提高了各类生物炭的比表面积和孔体积,增幅分别为2.70%～110.84%和1.42%～123.80%,提高其芳香性(C=C),H/C增幅为5.56%～29.41%,同时降低了极性官能团(C—O和C=O)含量,极性指数[(O+N)/C]降幅为13.18%～46.34%。原始生物炭的磷释放量范围为78.33～568.33 mg·kg^-1,NaHCO₃前处理显著增加各类生物炭对磷的吸附,使其表现出近似的磷吸附能力(Freundlich吸附系数K_F范围为119～254 mg^1-n·Lⁿ·kg^-1)...     

Persistence of tebufenozide in aquatic ecosystems under laboratory and field conditions

The persistence and dissipation behaviour of tebufenozide, an ecdysone agonist, were investigated: (1) under laboratory conditions in aquatic models set up in glass aquaria, and (2) under field conditions in in-situ aquatic enclosures deployed in a mixed-wood boreal forest lake. Two models were set up in the laboratory study (Study I), which was conducted at constant conditions of temperature, water pH and photoperiod. In Model I, partitioning of tebufenozide from sediment, treated at a concentration of 1400 μg kg^-1, into untreated water was examined. The results showed that the chemical moved very little from the treated sediment into water. The concentration in sediment and water decreased gradually during the 90-day incubation period. Tebufenozide disappeared faster from the top layer of sediment than from the middle and bottom layers. The half-lives of disappearance were 64 days for the top layer but >90 days for the middle and bottom layers respectively. In Model II, partitioning from water, treated at a concentration of 350 μg litre^-1, into untreated sediment was investigated. The results showed that the chemical moved from treated water into sediment due to adsorption. Little vertical downward movement of the adsorbed residues from the top layer of sediment occurred into layers beneath. The adsorbed residues were also not released readily back into water. The concentration in water and sediment decreased gradually during the 90-day incubation period. The half-life of dissipation from water was 67 days. The field microcosm study (Study II), conducted under fluctuating conditions of temperature, water pH and photoperiod, involved application of tebufenozide onto aquatic enclosures at four concentrations of 0·05, 0·10, 0·26 and 0·5 mg litre^-1. This study also showed that the chemical moved downwards from the applied location and was adsorbed onto sediment. The chemical persisted longer in Study II than in Study I. Tebufenozide, being photo-labile, probably degraded faster after constant exposure to light in Study I than after exposure to fluctuating light in Study II. At 90 days after treatment in Study I, only about 55% of the applied material persisted in the sediment, and there was little accumulation. In Study II, the material not only persisted but also was accumulated in the sediment, since at 92 days post-treatment the residues were about 25 times higher than the applied concentration level. Residues in water also decreased more rapidly in Study I than in Study II, because the concentration at 90 days post-treatment was about 41% of the applied value. In Study II, however, about 65% of the applied chemical persisted in water at 92 days post-treatment. While the long persistence of tebufenozide in both the laboratory and field studies was attributable to its low vapour pressure, low water solubility, high octanol/water partition coefficient etc., the differences in the persistence characteristics observed in the two studies were due to the fluctuating environmental conditions and water pH encountered in the field study, compared with the constant environmental conditions and water pH utilized in the laboratory study. © 1997 SCI.     

The Magnesium Status of Some Fiji Soils

Abstract

Magnesium (Mg) is an essential macronutrient element for all living organisms, but literature reports of Mg deficiency in agriculture and forestry appear regularly. In many tropical areas, Mg is added to soils by using dolomitic limestone and as minor additions through impurities in some fertilizers. Minimal information is available on the Mg status of Fiji soils, and deficiencies have been observed in some crops. This study investigated the Mg status of a range of Fiji soils and found that major agricultural soils of Fiji contain variable amounts of Mg, both in the total concentrations and in the different forms of the element present. The variations can be related to the soil parent materials, degree of weathering, clay content, and mineralogy. Low plant‐available Mg concentrations are present in many of the highly weathered soils with limited reserves present. Development of intensive agriculture should consider Mg when developing fertilizer programs.     

The severity of smouldering peat fires and damage to the forest soil

Smouldering wildfires propagate slowly through surface and subsurface organic layers of the forest ground and severely affect the soil, producing physical, chemical and biological changes. These effects are caused by the prolonged heating and the large loss of soil mass but are poorly documented in the literature. A series of smouldering experiments with boreal peat have been conducted under laboratory conditions to quantify these effects using small-scale samples. Peat samples of 100 mm by 100 mm in cross section and 50 mm in depth of different moisture were exposed to an external ignition source. Thermocouples placed throughout the sample bed measured the temperature evolution and tracked the peat ignition, intensity and spread of the smouldering front. The results show that moisture content controls peat ignition and that moisture below 125 ± 10% (in dry base) are required. The severity of the smouldering peat on the soil has been quantified in terms of temperature vs. residence time curves and mass loss. The measurements show temperatures in excess of 300 °C for residence times of 1 h leading to sterilization of the soil and mass loss in burnt layers above 90%.     

含水量与包装方法对大黄品质的影响

通过观察比较不同含水量和包装方法下大黄的外观及品质变化,探寻一种经济实用的大黄包装储藏方法。结果表明,大黄最佳包装条件为含水量16%～18%时采用抽真空包装。该条件下大黄未发生霉变,质量损耗为2.79 g;蒽醌含量可达1.89%,浸出物含量可达31.50%。     

几种有机酸对恒电荷和可变电荷土壤吸附Cu2+的影响

以恒电荷土壤(黄褐土和黄棕壤)和可变电荷土壤(红壤和砖红壤)为供试材料,研究了乙酸、草酸、酒石酸和柠檬酸对土壤吸附重金属铜离子(Cu2 )的影响。结果表明,在相同酒石酸浓度下,土壤对酒石酸的吸附量依次为黄棕壤(2 1 8mmolkg-1) >红壤(15 4mmolkg-1) >砖红壤(9 5mmolkg-1) ,土壤吸附有机酸后负电荷量增加,相同条件下增幅为砖红壤>红壤>黄棕壤;无有机酸配体时,供试土壤对Cu2 的吸附量为黄褐土>黄棕壤>砖红壤>红壤;加入有机酸时,随有机酸浓度增高,土壤对Cu2 的吸附一般表现为“峰”形曲线,峰所对应的有机酸浓度因有机酸类型而异,且随土壤可变电荷性质增强而增高;土壤吸附有机酸后对Cu2 的次级吸附不同于有机酸与铜共存时的竞争吸附,且因土壤性质表现迥异。这些结果意味着在存在有机酸配体的根际环境中,恒电荷土壤与可变电荷土壤对Cu2 的吸附明显不同,并将影响重金属离子在根际的转化与有效性     

基于响应曲面法探究糠醇改性对处理材吸湿性的影响

基于响应曲面法探究了马来酸酐浓度、四硼酸钠浓度和溶液静置时间对糠醇处理材吸湿性的影响。结果表明:(1)各因素对糠醇处理材吸湿性的影响程度为:四硼酸钠浓度>马来酸酐浓度>溶液静置时间。其中,四硼酸钠浓度和马来酸酐浓度具有显著性影响,且两者交互作用对吸湿率影响较大;溶液静置时间的影响不显著。(2)糠醇处理材的吸湿率随马来酸酐浓度增大,呈现先降低后升高的趋势;而四硼酸钠浓度增加,糠醇溶液虽然储存稳定性提高,但导致处理材吸湿性增大。(3)优化工艺条件为:马来酸酐浓度3.02%,四硼酸钠浓度1.03%,溶液静置时间3.8h。吸湿率的预测值与实验值误差约1%,预测效果较好。     

基于近红外预测羊草水分含量的特征光谱模型研究

水分是牧草最为重要的品质属性,水分含量的多少直接影响牧草品质的变化。羊草（Leymus chinensis）因富含重要的维生素、蛋白质、中性洗涤纤维、酸性洗涤纤维、脂肪等家畜必需营养成分,在收获和储藏过程中极易受到生长地的水、土、气等的影响而发生营养成分损失或变质,因此为了有效降低冗余无信息变量,提高羊草水分含量近红外模型的预测精度和稳定性,本研究采用4种光谱特征区间选择方法,包括间隔偏二乘法（Interval partial least-squares regression,iPLS）、向后区间偏最小二乘法（Backward interval PLS,BiPLS）、联合区间偏最小二乘法（Synergy interval PLS,SiPLS）、和连续投影算（Successive projections algorithm,SPA）建立羊草水分含量的预测模型。结果表明：SiPLS方法最适合用于羊草水分含量特征波长的筛选,其次为BiPLS方法,最差的方法为iPLS,同时,相对分析误差（Residual predictive deviation,RPD）=2.648>2.50。这表明SiPLS的近红外光谱模型在预测羊草水分含量的应用上完全可行,预测精度在96.13%以上。     

饲料中几种主要霉菌毒素的危害及防治措施

饲料霉变严重危害饲料业及畜牧业生产过程。就饲料中几种常见霉菌毒素的危害及防治措施进行了综述．并主要介绍了以生物防治为主的防治措施,以期为科学认识霉菌毒素和选用防霉剂提供参考依据。