农业资源利用模式间的转换及案例分析

目前我国农业仍然属于资源高耗低效型农业，而农业自然资源是非常有限的，为此必须实现农业资源的高效利用。本文从中观区域尺度上研究了农业资源利用模式及不同利用模式间的转换，通过案例分析认为，农业资源利用模式处于不断演替过程中，其演替具有明显的层次性；在演替过程中，物化资源投入水平不断增加，农业资源利用效率不断提高；与农业资源利用模式相适应的农业资源利用技术体系也具有多样性和层次性。     

亚铵制浆黑液非无菌操作连续发酵生产酵母

从土壤中筛选出能在亚铵黑液中生长的毕赤酵母菌株（Ｐｉｃｈｉａ ｓｐ．Ｎｏ．１）经耐毒驯化后，可接种于酸析脱木素和汽提脱毒后的亚铵黑液中，在非无菌操作条件下连续发酵生产酵母菌体，该菌生产迅速，连续培养衡释率达０．２６ｈ＾－１，总糖的酵母得率为０．４８ｇ／ｇ（ＴＳ），ＣＯＤ去除２３％，菌体易絮凝，可自然沉降分离。     

我国东部冲积平原区水成土壤元素背景值地域分异规律

从气候条件、母质物质组成的差异以及河流上下游物质之间的联系等角度，讨论了我国东部冲积平原区土壤中１３种元素的地理分布趋势及影响因素。研究表明，大多数元素具有明显的南北向地域分布趋势，这种趋势是地带性和非地带性因素共同决定的，而以非地带因素更重要。此外，东部平原土壤与相应主要河流上游侵蚀区土壤微量元素含量具有很好的共轭关系。     

用水基表面活性剂乳液回收废白土中蜡的界面张力研究

通过测定液体与废白土粉末之间的接触角及液体与蜡之间的液液界面张力，对水基表面活性剂乳液的溶剂及配方进行了优选，得到最佳的水基面活性剂乳液的组成为：质量分数０．２％的十二烷基苯磺酸钠＋体积分数为２．５％的乙醇＋体积分数为２５％的混合烃（正己烷＋苯，等体积）＋体积分数为７２．５％的水。实验证明，用该水基表面活性剂乳液处理废白土，蜡的回收率可达８０％，同时不破坏白土的颗粒结构。     

小麦发芽期锌的毒害作用和钙的去毒害作用研究

试验表明,较高浓度的Zn~(2+)对小麦种子的发芽和α-淀粉酶的活性有抑制作用.设置了胚芽鞘长/胚芽鞘粗和主胚根长/主胚根粗两项相对生长指标,发现:随Zn~(2+)处理浓度的提高,两项指标均逐渐下降.饱和CaCO_3和0.5％CaCl_2溶液对80ppmZn~(2+)处理过的小麦幼苗的毒害具一定解毒作用.对Ca~(2+)和pH条件与种子发芽时的形态建成和α-淀粉酶活性之间的关系进行了讨论.     

Study on nitrile-degrading microorganisms

Two strains of bacteria were isolated from nitrile polluted soils, and identified as Corynebacterium boffmanii and Arthrobacter flavescens. Acetonitrile, propionitrile, butyronitrile and acrylonitrile were degraded by these bacteria to yield corresponding amides, carboxylic acids and ammonia. The nitrile-degrading abilities of these strains were investigated. The removal rates for the nitrile were nearly 100%, after these bacteria were grown in medium containing 10000 ppm of aceto-, propio-, or butyronitrile at 28 ℃ for 24h. When the reaction mkture consisting of 5000 ppm of above mentioned nitriles or acrylonitrile and 20g (dry cell) /L resting cells of the two strains in 0.06mol/L phosphate buffer (pH7.5) was incubated separately at 25 ℃ with moderate shaking for 15 or 45 min, the nitrile could be degraded completely. The optimum growth conditions for C.hoffmanii and A.flavescens were studied as well.     

Sensitivity experiments and assessment of climatic changes in China induced by greenhouse effect

Climatic changes can be separated into two parts: natural changes -and human activity influenced on climatic changes. The observed data could not only show the effects caused by human activity. Several simulated results as simulated by the GCMs induced by the greenhouse effects in China .have been analysed. It is shown that an obvious warming of about 3-6℃ in winter and 2-5℃ in summer in China as simulated by the GCMs induced by doubling CO2 have been found. There are getting drier or wetter regions in China due to doubled CO2 as simulated by most of models. Comparing the simulated results with the observed data in China, some simulated results are able to be believed. The GCMs should be improved, especially in the regional areas.     

北京平原土壤中若干元素背景含量的区域分异

本文根据计算机绘制的北京平原地区土壤元素等含量线图和趋势面图,揭示了土壤元素的区域分异规律,并对其引起区域分异的环境因素进行了分析。     

土壤的重金属污染与土壤酶活性

本文根据模拟研究,论述了不同用量的重金属Hg、Cd和Pb对不同肥力水平的棕壤和红壤的过氧化氢酶、转化酶、脲酶和磷酸酶活性的影响.重金属对土壤酶抑制作用的顺序为:Hg>Cd>Pb.且随金属浓度的增大而增强.实验表明,重金属对土壤酶活性的抑制是一种暂时现象、由于脲酶活性恢复得较少较慢,故建议用土壤的脲酶活性作为土壤Hg污染程度的指标.