微波辅助提取山黄皮果中的黄酮类物质

[目的]确定从山黄皮[Clausena indica（Datz）.Oliv.]果中提取黄酮类化合物的优化条件。[方法]通过单因素试验和正交试验对微波辅助提取山黄皮黄酮类化合物的工艺条件进行了探讨,研究了溶剂浓度、料液比、微波功率及微波处理时间对黄酮类化合物提取的影响;并对微波辅助提取法和常规提取法的效果进行了比较。[结果]山黄皮果中黄酮类化合物微波辅助提取的最佳条件为：乙醇体积分数60%,料液比1∶50,微波功率240W,微波处理时间60s,在此条件下,提取所得山黄皮中黄酮类化合物含量为3.621%,常规提取法提取所得黄酮类化合物含量为3.216%。[结论]微波辅助法提取山黄皮果中的黄酮类物质效果优于常规提取法。     

亚硝酸盐氮对克氏原螯虾仔虾的急性毒性效应

研究了亚硝酸盐氮对克氏原螯虾(Procambarus Clarkii)仔虾的急性毒性效应,结果表明:克氏原螯虾仔虾对亚硝酸盐氮的耐受性随接触时间的增加而明显降低;亚硝酸盐氮对克氏原螯虾仔虾24 h、48 h、72 h、96 h半致死浓度分别为28.69 mg/L、22.69 mg/L、18.92 mg/L、15.19 mg/L,安全浓度为1.52 mg/L.     

Grain legume effects on soil nitrogen mineralization potential and wheat productivity in a Mediterranean environment

The objective of this work was to provide evidence on the effects of faba bean (Vicia faba L.) and chickpea (Cicer arietinum L.) on the dynamics of soil N availability and yield parameters of wheat (Triticum turgidum L. var. durum) in a legume–wheat rotation in comparison with the effects of the more extensively studied common vetch (Vicia sativa L.). Soil samples were taken from field plots just before wheat sowing and incubated in the laboratory to assess N mineralization potential, soil respiration and N immobilization after incorporation of legume residues. Soil after vetch cultivation showed the highest residual N and mineralization potential (120 mg N kg^?1 soil), the greatest CO₂ release and the smallest N immobilization. Smaller mineral N release (80 mg N kg^?1 soil) was shown by soil after faba bean cultivation, which, however, would be capable to support an average wheat production without fertilization. Soil after chickpea and wheat cultivation manifested no differences in residual N and mineralization or immobilization potential. Laboratory results were well correlated with grain yield and N uptake during the second season of rotation in the field. All legumes resulted in significant yield surpluses and provided N credit to the following unfertilized wheat.     

几种丛生竹根际联合固氮研究

对几种丛生竹种麻竹、吊丝球竹、青皮竹、粉丹竹、马甲竹、绿竹等进行根系固氮能力调查测定 ,用直接法测定 (干根样品 )前 5个种竹种的根系最高固氮酶活性分别为 2 0 .50、2 4 .81、10 .83、7.4 9、2 .4 6nmol(C2 H4 )·g- 1·h- 1,用富集培养法测定 (鲜根样品 )前 5个种竹种的根系平均固氮酶活性分别为 2 75、4 31、169、188、79nmol(C2 H4 )·g- 1·h- 1。不同生境和不同季节丛生竹根系固氮能力的调查显示 ,充足的水分供应、较高的温度及适当施用有机肥有利于竹子固氮。对几种丛生竹种根际不同部位固氮菌数调查测定显示 ,根际固氮菌数最多的竹种是吊丝球竹 ,在根际不同部位固氮菌数由非根际土→根际土→根表→根内依次急剧递增 ,越往内部根际效应越明显。用 2 #、12 #、14#、7#菌及混合菌液对麻竹组培苗进行接种显示 ,接种固氮菌可提高苗木成活率和植株含氮量 ,14#、7#菌和混合菌接种可显著提高麻竹组培苗生物量。     

不同草地利用方式对土壤有机碳、全氮和全磷的影响

以青海省共和县塔拉滩封育芨芨草(Achnatherum splendens)草原、过牧芨芨草草原、取土坑、人工草地和农田为研究对象,对不同利用方式及不同深度下土壤有机碳、全氮、全磷含量进行了分析研究。结果表明:0～10cm和10～20cm土层土壤有机碳含量顺序均为封育芨芨草草原>退化过牧芨芨草草原>取土坑>农田>人工草地,说明退化和开垦均导致表层土壤有机碳含量的下降。在同一土层内,农田和人工草地(退耕地)的有机碳含量差异不显著(P>0.05)。在0～10,10～20和20～40cm的3个土层,农田的全氮含量最高,人工草地次之,主要是由于人为施加氮肥和翻压枯草等因素造成,取土坑的全氮含量最低;同时,0～40cm的土层,封育芨芨草草原的土壤全氮含量高于退化过牧芨芨草草原,40～80cm的土层,封育芨芨草草原的土壤全氮含量低于退化过牧芨芨草草原,说明封育使土壤上层的全氮含量增加,而草原退化导致氮向下层转移。全磷含量的变化规律与全氮相似。各草地的有机碳、全氮和全磷含量随土壤深度增加而下降。     

调亏灌溉和氮处理对小桐子生长及水分利用的影响

为了研究阶段水分亏缺(亏水+不亏水W_LW_H、不亏水+亏水W_HW_L、亏水+亏水W_LW_L、不亏水+不亏水W_HW_H)和不同施氮量(N_Z:0,N_L:0.2 g/kg,N_H:0.4 g/kg)对小桐子生长、生理指标和灌溉水利用效率的影响,通过盆栽试验,发现W_LW_H的生长和灌溉水利用效率均显著高于W_HW_L;作物的灌溉水利用效率随施氮量的增大而呈现先增大后减小的趋势,在N_L水平下达到最大值;与高水高氮的处理N_HW_HW_H相比,中水低氮处理N_LW_LW_H节约灌溉水27%,节约氮肥使用量50%,小桐子株高减少31%、总干物质量减少35%,灌溉水利用效率减少13%,但茎粗增加13%,根冠比增加20%.可见小桐子在第一阶段处理(40~90 d)幼树期对水分的需求量较小,适度的亏缺灌溉可提高灌溉水利用效率;小桐子在第二阶段处理(90~140 d)处于旺长期,对水分的需求量较大,增大灌水量可大幅度促进小桐子生长及其干物质量的积累.全生育期实施亏缺灌溉,可提高小桐子自身适应外界环境能力,抗干旱胁迫能力也逐渐增强,但W_LW_L水平下的小桐子生长缓慢.经综合分析,认为处理N_LW_LW_H可作为干旱地区条件下的小桐子灌溉和施氮制度.     

Simulation of drainage water quality with DRAINMOD

The design and management of drainage systems should consider impacts on drainage water quality and receiving streams, as well as on agricultural productivity. Two simulation models that are being developed to predict these impacts are briefly described. DRAINMOD-N uses hydrologic predictions by DRAINMOD, including daily soil water fluxes, in numerical solutions to the advective-dispersive-reactive (ADR) equation to describe movement and fate of NO₃-N in shallow water table soils. DRAINMOD- CREAMS links DRAINMOD hydrology with submodels in CREAMS to predict effects of drainage treatment and controlled drainage losses of sediment and agricultural chemicals via surface runoff. The models were applied to analyze effects of drainage intensity on a Portsmouth sandy loam in eastern North Carolina. Depending on surface depressional storage, agricultural production objectives could be satisfied with drain spacings of 40 m or less. Predicted effects of drainage design and management on NO₃-N losses were substantial. Increasing drain spacing from 20 m to 40 m reduced predicted NO₃-N losses by over 45% for both good and poor surface drainage. Controlled drainage further decreases NO₃-N losses. For example, predicted average annual NO₃-N losses for a 30 m spacing were reduced 50% by controlled drainage. Splitting the application of nitrogen fertilizer, so that 100 kg/ha is applied at planting and 50 kg/ha is applied 37 days later, reduced average predicted NO₃-N losses but by only 5 to 6%. This practice was more effective in years when heavy rainfall occurred directly after planting. In contrast to effects on NO₃-N losses, reducing drainage intensity by increasing drain spacing or use of controlled drainage increased predicted losses of sediment and phosphorus (P). These losses were small for relatively flat conditions (0.2% slope), but may be large for even moderate slopes. For example, predicted sediment losses for a 2% slope exceeded 8000 kg/ha for a poorly drained condition (drain spacing of 100 m), but were reduced to 2100 kg/ha for a 20 m spacing. Agricultural production and water quality goals are sometimes in conflict. Our results indicate that simulation modeling can be used to examine the benefits of alternative designs and management strategies, from both production and environmental points-of-view. The utility of this methodology places additional emphasis on the need for field experiments to test the validity of the models over a range of soil, site and climatological conditions.     

Influence of race and crossbreeding on casein micelles size

Casein (CN) micelles are colloidal aggregates of protein dispersed in milk, the importance of which in the dairy industry is related to functionality and yield in dairy products. The objective of this work was to investigate the correlation of milk CN micelles diameter from Holstein and Zebu crossbreds with milk composition (protein, fat, lactose, total and nonfat solids and milk urea nitrogen), somatic cell count (SCC), age, lactation stage and production. Average casein micelles diameters of milk samples obtained from 200 cows were measured using photon correlation spectroscopy and multiple regression analysis was used to find relationship between variables. CN micelle diameter, SCC and nonfat solids were different between animals with different Holstein crossbreed ratios, which suggests influence of genetic factors, mammary gland health and milk composition. Overall, results indicate the potential use of CN micelle diameter as a tool to select animals to produce milk more suitable to cheese production.     

Chemically and biologically activated biochars slow down urea hydrolysis and improve nitrogen use efficiency

Biochar is considered a potential technology to enhance chemical fertilizer use efficiency through intensification of the interactions between nutrients and the functional groups on biochar surfaces. However, little is known about how the application of activated biochars mixed with urea influences nitrogen(N) mineralization and crop performance in paddy fields. Here, a sawdust-derived fresh biochar (FBC)(ca. 400?C) was activated chemically with 15%hydrogen peroxide and biologically with a nutri...     

石灰性土壤供氮能力几种化学测定方法的评价研究

以采自于黄土高原差异较大的25个农田耕层石灰性土壤为供试土样,以淋洗和未淋洗土壤起始NO3--N小麦和玉米两季盆栽试验作物累积吸氮量为参比,对8种反映旱地土壤供氮能力的化学方法进行比较研究。结果表明,在一定程度上,可用有密切关系的土壤全氮或有机质,反映有机氮或全氮存在较大差异的土壤供氮能力,但其灵敏性较差。石灰性土壤矿质氮,特别是NO3--N与未淋洗土壤起始NO3--N作物吸氮量之间有较高相关性(r=0.884,P0.01),而与淋洗土壤起始NO3--N作物吸氮量间相关系数仅为0.472(P0.05),说明矿质氮可反映土壤当前供氮水平,而不能反映土壤潜在供氮能力;石灰性土壤起始NO3--N对各化学方法与作物吸氮量之间相关性影响较大。酸性高锰酸钾法既可反映土壤潜在供氮能力,也可反映土壤总供氮能力;酸性高锰酸钾法的修订方法,即硫酸高锰酸钾法提取出的NH4+-N值接近于KCl水浴法提取出的NH4+-N值,该方法在反映土壤总供氮能力方面与酸性高锰酸钾法相当,但在反映土壤潜在供氮能力方面不及酸性高锰酸钾法优越。KCl水浴法在评价石灰性土壤供氮能力方面,与酸性高锰酸钾法的效果基本相同;沸水浸取法和NaHCO3-UV法在评价石灰性土壤供氮能力方面效果较差。总结以上发现,在以盐类溶液提取法中,酸性高锰酸钾法、硫酸高锰酸钾法和KCl水浴法可作为反映石灰性土壤供氮能力的化学方法,其中以酸性高锰酸钾法最优,其次为KCl水浴法和硫酸高锰酸钾法。这3种方法在不包括起始NO3--N时,可反映石灰性土壤潜在供氮能力;包括起始NO3--N后,可反映土壤总供氮能力(当前供氮能力+潜在供氮能力)。