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991.
低能离子注入对大豆酯酶同功酶活性的影响   总被引:3,自引:1,他引:3  
利用 30KeV低能氮离子在 3× 10 15~ 3× 10 17N+ ·cm-2 剂量范围内对大豆进行了离子注入 ,并用电泳结合薄层扫描的方法对其酯酶同功酶的相对活性进行了测定 .结果表明 ,其变化为升 降 升 降的振荡型变化趋势 .真空对照样品的电泳结果显示 ,酶活性随真空时间变化略呈上升的趋势  相似文献   
992.
993.
The design of multi-controller and multi-mode control law is presented for the three-link Acrobot on horizontal bar by employing Human simulated intelligent control method based on sensory-motor Schema.Imitated the characteristics of gymnast's swing-up and handstand movement,the control process of robot is divided by six sequence phase.Then the sensory cell and motor cell and the group of sensory-motor schema is designed based on the analysis of quality-quantity combination.The simulation results show that the controller ensures the gesture and the energy to the desired goal,farther more the motion control of giant swing backword is realized in the simulation.  相似文献   
994.
A theoretical model is developed for the dropwise condensation heat transfer on the horizontal circular surface with radial gradient surface energy based on the heat transfer model of individual condensate drop and the size distribution model of condensate drop on homogeneous condensation surface.The effect of variation of contact angle on the gradient surface on condensation heat transfer and condensate drop size distribution is taken account of in this model.The theoretical calculation method was obtained to predict the dropwise condensation heat transfer coefficient on the horizontal circular surface with radial gradient surface energy under various wall subcooled temperature,contact angle profile on wall surface,and working fluid.The effects of surface energy gradient,wall subcooled temperature,and thermophysical properties of condensate on the condensation heat transfer are discussed respectively.The calculation results show that the condensation heat transfer coefficient increases slightly with the increase of wall subcooled temperature.As latent heat and surface tension increasing,the condensation heat transfer coefficient increases.A larger surface energy gradient induces a larger condensation heat transfer coefficient.  相似文献   
995.
Credit risk, the major risk of bank, is more and more intense during the period of economic restructuring in China. In view of the flaw of present risk measurement system, Conditional Value-at-Risk is used for the credit risk measurement which is better than Value-at-Risk. This paper creates the model ,while gives the method and procedure for solving it. So CVaRof credit combination is produced, which is just the early warning value of credit risk. At last, it is concluded that the CVaRrisk measurement is too difficult to use widely at present in china, then some advice is provided.  相似文献   
996.
The agent - construction system, as a new public project management mode, has been practiced in some cities and attracted attention from the society. This paper firstly studies the features and operation modes of agent - construction system, and discusses the agent - construction system from the viewpoints of promoting competition, nourishing agent -construction enterprises, setting up a supervisory and encouraging mechanism, and its connection with the governmental project procurement system etc.  相似文献   
997.
2012年9月至2013年8月,利用包裹式树干液流仪、插针式树干液流仪和小气象站对南京市东善桥林场的杉木幼树树干液流速率、杉木树干液流速率及环境因子进行了连续观测,研究了杉木幼树树干液流影响因子及其对杉木林蒸腾的贡献。结果表明:(1)杉木幼树液流速率的日变化具有季节差异性,均表现为单峰曲线并且日间液流速率大于夜间;(2)春、夏、秋、冬季液流速率峰值分别为:79.97,105.22,70.30,33.19g/h;(3)太阳辐射是影响杉木幼树树干液流速率的主导因子,其次是饱和水汽压差,日液流量与太阳辐射、空气温度、饱和水汽压差、各层次土壤温度呈极显著的正相关关系;(4)分别建立了液流速率、日液流量与环境因子的模型,可以较好地解释液流速率与日液流量的变化;(5)杉木幼树全年液流量对杉木林蒸腾量的贡献率为6.12%,夏季的贡献率最大。  相似文献   
998.
以1986,1996,2011年的TM影像为数据源,利用基于GIS和遥感技术的景观指数分析法研究皖西退耕还林重点地区--金寨县的森林景观格局演变特征及其内在驱动机制。结果表明,25 a间,金寨县林地面积持续增加,耕地面积不断减少,其他景观类型面积的增减幅度不同。1986-1996年,斑块密度、分形维数、香农均匀度等指标发生负向变化,景观异质性速度加快,景观格局复杂化和破碎化形势严峻;1996-2011年,退耕还林工程实施后,各项指标发生正向变化,景观格局破碎化形势得到有效遏制,景观格局向规则化和均衡化转变,景观结构明显优化。自然地理环境和退耕还林工程的实施是该县森林景观格局演变特征形成的主要驱动力。  相似文献   
999.
Located in the inland arid area of central Asia, salt-affected farmlands take up one third of the total irrigated land area in Xinjiang of Northwest China. Spatio-temporal variability of soil salinity and the underlying mechanism are fundamental problems challenging the sustainability of oasis agriculture in China. In this study, the data of total dissolved solids(TDS) measured for soil samples collected from 27 representative study areas in the oasis areas of Xinjiang were analyzed and the coefficient of variation(CV) and stratification ratio(SR) of TDS were used to describe the lateral and vertical soil salinity variations, respectively. Weekly, monthly,and annual changes in soil salinity were also summarized. Results showed that the top(0–20 cm) soil salinity was highly variable(CV 75%) for most studied areas. Lateral variation of soil salinity was significantly correlated with the sampling interval; as a result, a maximum sampling interval of 0.9 m was found for reducing evaluation uncertainty. The top 0–20 cm soil salt accounted for about25.2% of the total salt in the 0–100 cm soil profile. The stratification ratio values(the ratio of TDS at the 20–40 cm depth to that at the 0–20 cm depth) were mostly smaller than 1 and on average 0.92, illustrating that the top 0–20 cm soil contained slightly more salt and a considerable amount of salt still existed in subsurface and deep horizons. Irrigation reduced top soil salinity by 0.52 g kg-1, or14.6%, within the first week. On average, the relative range of soil salinity, calculated to indicate monthly changes in soil salinity, was58.2% from May to September. A 27-year experiment indicated that cultivation increased soil salinity by 44.4% at a rate of 0.14 g kg-1year-1. At small spatio-temporal scales, soil salinity variation was mainly affected by anthropogenic factors, such as irrigation and land use. However, natural factors, including groundwater, topography, and climate conditions, mainly influenced soil salinity variation at large spatio-temporal scales. This study displayed the highly variable nature of soil salinity in space and time. Those driving factors identified in this study could provide guidelines for developing sustainable agriculture in the oasis areas and combating salinization in arid regions of China.  相似文献   
1000.
横、顺坡垄作对黑土坡面侵蚀-沉积周期规律的影响   总被引:3,自引:0,他引:3  
王小康  谷举  刘刚  师宏强 《土壤学报》2022,59(2):430-439
我国东北黑土区的水土流失和土地退化正严重制约着东北地区农业经济发展,威胁国家粮食生产安全。掌握不同垄作方向耕作措施下的东北黑土区土壤侵蚀规律,对合理布设水保措施、控制水土流失等具有重要意义。采用137Cs示踪技术并结合小波分析方法,对不同垄作方向坡耕地土壤侵蚀-沉积速率的空间变化规律开展研究。结果表明:(1)横、顺坡垄作坡面137Cs平均浓度分别为1 802 Bq·m-2和1 770 Bq·m-2,均小于当地背景值2 417 Bq·m-2,说明在两种垄作方向下均发生了不同程度的土壤侵蚀。(2)横坡垄作的坡面平均侵蚀速率(1 341 t·km-2·a-1)小于顺坡垄作(1 477 t·km-2·a-1),表明在长期平均条件下前者的水土保持作用优于后者。尽管研究区土壤侵蚀属于轻度侵蚀,但其侵蚀速率远大于黑土区的土壤容许流失量(200 t·km-2·a-1  相似文献   
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