适宜无机盐及浓度抑制麦胚脂肪酶存在时油水界面张力

为了探明无机盐稳定化脂肪酶的潜在机理,该文以小麦胚芽脂肪酶为研究对象,基于界面酶学的分析方法,研究添加浓度介于1.0×10-9~1.0×10-2 mol/L的Na~+、K+、Ca~(2+)、Mg~(2+)的氯化物对小麦胚芽脂肪酶存在的油-水界面特性的影响。结果表明,当小麦胚芽脂肪酶体系浓度为1.7×10-6 mol/L时,一价金属中Na~+更有利于抑制油-水界面的表面张力(P0.05),对麦胚脂肪酶存在时的油水界面特性影响也较大;二价金属离子Ca~(2+)对界面张力的影响趋势与一价离子不同,在高浓度时反而增加界面张力;当油水界面上存在脂肪酶的催化底物(三油酸甘油酯)和产物(油酸)时,添加浓度分别为10-6、10-6、10-4和10-9mol/L的Na~+、K~+、Ca~(2+)、Mg~(2+)均可一定程度上降低油水界面张力,从而降低麦胚脂肪酶的作用效果,三油酸甘油酯存在时Mg~(2+)的作用效果最明显(P0.05),油酸存在时Na+的作用效果最明显(P0.05)。综上,无机盐金属离子主要通过影响麦胚脂肪酶在油水界面的聚集行为及底物结构状态起到钝化麦胚脂肪酶的作用,该结果可为麦胚脂肪酶存在时界面的活性调控及麦胚的稳定化处理提供参考。     

九宫山土壤剖面中黏土矿物的组成特征

以湖北省九宫山的4种垂直地带性土壤为对象,研究其剖面层次的黏土矿物组合和铁、铝氧化物的特征,揭示山地土壤中黏土矿物的变化特点。结果表明,随海拔升高,土壤中黏土矿物类型从以高岭石为主,逐渐变为以14.0?矿物、伊利石及三水铝石为主,有从1︰1型向2︰1型矿物过渡的趋势;不同层次的土壤中黏土矿物类型和相对含量变化明显;土壤随垂直高程的升高,其中游离态铁、铝减小,非晶形和络合态铁、铝增加,各种形态铁、铝氧化物的总量也增加。     

中国福建省土壤的主要粘土矿物

The clay minerals of more than 200 soil samples collected from various sites of Fujian Province were studied by the X-ray diffraction method and transmission electron microscopy to study their distribution and evolution.Montmorillonite was found in coastal solonchak,paddy soils derived from marine deposit,lacustrine deposit and river deposit,and some lateritic red soil,red soil and yellow soil with a low weathering degree.Chlorite existed mainly in coastal solonchak and paddy soil developed from marine deposit.1.4nm intergradient mineral appeared frequently in yellow soil,red soil and lateritic red soil.The content of 1.4nm intergradient mineral increased with the decrease of weathering degree from lateritic red soil to red soil to yellow soil.Hydrous micas were more in coastal solonchak,paddy soils derived from marine deposit,lacustrine deposit and river deposit.and puple soil from purple shale than in other soils.Kaolinte was the most important clay mineral in the soils iun this province.The higher the soil weathering degree,the more the kaolinite existed.From yellow soil to red soil to lateritic red soil,kaolinite increased gradually,Kaolinite was the predominant clay mineral accompanied by few other minerals in typical lateritic red soil. Tubular halloysite was a widespread clay mineral in soils of Fujian Province with varying quantities.The soil derived from the paent rocks rich in feldspar contained more tubular halloysite.Spheroidal halloysite was found in a red soil and a paddy soil developed from olivine basalt gibbsite in the soils in this district was largely“primary gibbsite” which formed in the early weathering stage.Gibbsite decreased with the increase of weathering degree from yellow soil to red soil to lateritic red soil.Goethite also decreased in the same sequence while hematite increased.     

乳汁草引种试验研究

乳汁草是一种新的适于我国南方生长的水土保持草种。在江西红壤丘陵区的引种试验表明 ,乳汁草年产鲜草5 9 6t/hm2 ,干物质粗蛋白含量 13 6%～ 16.2 %,干物质粗纤维含量 2 1 6%～ 2 5 .6%,草质优 ,产量高 ,保持水土能力强。     

亚热带小流域不同沉积区土壤粘粒矿物的演变

在亚热带丘陵河谷地小流域范围内地表物质的迁移常可导致不同沉积区物质组成的变化 .从黄泥土→洪积泥砂土→培泥砂土 ,随着搬运距离的增加 ,其粘粒矿物组成发生了一系列的变化 ;高岭石逐渐下降 ,云母逐渐增加 ,蛭石渐趋下降消失 ,而绿泥石则逐渐形成 ;同时赤铁矿、针铁矿也先后下降消失 .矿物的演化与沉积物所处环境的水分条件及溶液中盐基物质和酸碱度变化有关     

草类物料压缩试验研究中的突破性进展

在国内外草物料压缩试验研究的基础上,对新鲜草物料压缩流变进行试验研究,总结出了草物料压缩试验研究过程中几个带有突破性的进展,较系统地展示了草物料压缩研究逐步深入的历程和规律,对草物料压缩基础研究的发展有重要意义。在国外研究“闭式压缩”很长时间后,我国开始了“开式压缩”试验研究。从实验室的局部过程的试验研究,发展到压缩工程全过程的试验研究;从一般工程力学的研究,推进入到压缩过程流变学试验研究;从理论上的阶跃历程的流变学试验研究,跨越到工程上任意历程的流变学试验研究,将草物料压缩流变研究推向新阶段。最后又提出了变断面积的压缩流变试验研究,继续推进草物料压缩工程和草物料加工流变学发展。     

铜和邻苯二胺在水相中和矿物上交互作用的研究

采用室内分析测定方法，研究了铜和邻苯二胺在水相以及高岭石和蒙脱石上的交互作用过程。结果表明，在纯水体系中邻苯二胺与铜发生了明显的络合反应，通过等摩尔法推导得出邻苯二胺与铜的络合系数为2，表观络合常数约在10^7数量级，且随酸度的变化而改变；邻苯二胺的存在降低了铜在高岭石上的吸附量；而在蒙脱石体系中，邻苯二胺的存在则增加了铜的吸附量，并随邻苯二胺浓度的增加这种作用更加明显。与此同时，邻苯二胺均降低了游离态铜在平衡溶液中的含量，而且铜的存在也相应降低了溶液中游离态邻苯二胺的浓度。该研究对于深入理解复杂体系中复合污染物之间交互作用过程具有一定的参考意义。     

不同钠浓度对白三叶草和多年生黑麦草生长的影响

白三叶草对Na 的反应比多年生黑麦草敏感.培养液中的Na 浓度从0.1mmol/L 增至0.5mmol/L 时,其干物质生产下降37%;增至2.5mmol/L 时,干重下降49%,而多年生黑麦草的干重仅降低6%.2种牧草的Na 含量均随培养液Na 浓度的增加而提高,K 含量未受影响.白三叶草的Na 含量低于多年生黑麦草,而K 含量高于多年生黑麦草.试验结果暗示,白三叶草对K 的选择吸收能力较多年生黑麦草强,但耐盐能力较差,生态适应性不如多年生黑麦草广.     

Herbage production,nutritive value and animal productivity within hardwood silvopasture,open and mixed pasture systems in Appalachia,United States

Demand for livestock food products is projected to increase dramatically through to 2050. Increased livestock production capacity on marginal lands will be critical to meeting this demand. A 5‐year research effort was undertaken to evaluate lamb and sward productivity within open and hardwood silvopasture (SP) systems in Appalachia, USA. Grazing began in mid to late April each year, with the grazing season averaging 141 d. Grazing system treatments during 2002 and 2003 grazing seasons were as follows: 100% open pasture (OP), 67% OP and 33% SP, and 67% OP and 33% SP with delayed SP grazing initiation (OSD). In 2004, a 100% SP (SP) system was added. Animals were rotationally stocked through either 6 (2002–2004) or 7 (2005–2006) paddocks. Open pasture produced greater (P < 0·001) grazing season herbage yield, while all systems generated similar animal performance. Based on summer solstice, herbage production in spring was greater (P < 0·001) than summer, except in 2003. Total non‐structural carbohydrate (TNC) content was greater (P < 0·05) in spring than in summer, except in 2004. Animal performance was superior in spring versus summer (P < 0·001). Animal plasma urea nitrogen (PUN) was lower (P < 0·05) for OP in 2003. When PUN was correlated with nutritive value indicators, the ratio of TNC to crude protein (CP) had the strongest correlation. The strong correlation indicates the need for synchronized ruminal energy and CP availability. Development of silvopasture from existing woodlots has potential to improve whole farm productivity on marginal lands.     

Simultaneous selection for seed and forage production in cocksfoot (Dactylis glomerata): application of drought tolerance and susceptibility indices

An experiment was conducted to estimate drought tolerance of some cocksfoot genotypes based on seed and forage yield and related indices (including tolerance index, mean productivity, geometric mean productivity, reduction percentage index, stress tolerance index and stress susceptibility index) and to identify relationships between measured traits. Twenty‐five genotypes were evaluated in the field under control and drought‐stress environments over 2 years. The results revealed a high variation for seed yield and forage yield and the measured indices under both moisture conditions. No correlation was observed between seed yield and forage yield under the control treatment, but this correlation was positively significant under the water‐stress treatment. Drought‐tolerant and susceptible genotypes were identified based on seed and forage yield performance. Genotypes 2, 4 and 7 had high seed yield, while genotypes 7 and 10 had high forage yield under both stressed and non‐stressed conditions and were identified as the most tolerant genotypes in each category. The results also revealed that genotypes 1, 2, 4, 6, 7, 8 and 24 had relatively high seed and forage yield in both control and drought‐stressed conditions. These genotypes can be used for further studies to improve both seed and forage yields concurrently.