Epicatechin can cause the seedling growth inhibitor,nagilactone E,to induce growth stimulation

Summary A possible new role for the flavonoid (–)-epicatechin (II) is described. It has no growth effects on its own, but when it is added to lettuce and rice seeds together with the known seedling growth inhibitor nagilactone E (I), the growth inhibitor activity ofI can cease and growth stimulation can be observed.     

果树滴灌自控系统的设计与试验

研究试验的滴灌自控系统,用于农田、果园、塑料大棚、温室及草坪绿地灌水,根据果树物候期的生长需要,可实现果园科学自动给水。本系统采用真空表张力计和光导纤维传感器,可做为普及推广滴灌和喷灌的配套设备。     

膜式机械通风横流冷却塔节能研讨

横流塔由于气水对数平均焓差较小。故在同参数下冷却数较逆流塔大,通常设计中电耗约高46％左右。本文从分析气流在填料中流态出发,探讨填料的相对凸起、风速与传质强度、能耗及投资间关系。由于在一定冷却数下,填料体积与传质强度成反比,前者与塔投资有关,后者当填料间距远小于其长度及高度时,可近似认为仅与填料形状及风速有关,即与能耗有关,故按投资回收期来选择填料形式并决定经济风速才是合理有效的节能方法。样塔提供较原塔节能65.7％的实例。本文亦可供膜式逆流塔参考。     

稻草制取多羟基化合物的探讨

本文探讨将农业废料稻草纤维素水解、发酵,制多羟基化合物的原理及方法。     

云南南沱组杂砾岩的成因及沉积相

作者对滇中震旦系,特别是下震旦统南沱组紫红色杂砾岩的成因和南沱期沉积相进行了较深入的研究,认为云南的南沱组杂砾岩既不是冰川搬运物质直接堆积的,也不是单纯的泥石流成因,而是兼具两者的某些特征。其沉积相的展布有从陆到海、从浅到深的特征。     

温度变化对牡丹花期影响的研究

通过几年来牡丹开花物候期２月至４月温度的观测与分析，探讨了牡丹开花物候期与旬平均气温、有效积温间的关系，并模拟了２月１０日后各物候期发育天数与其有效积温间的幂函数曲线模型，为牡丹适宜花期温度控制措施的制定提供了依据。     

后冷战时代印美关系的发展及动因

后冷战时代,印度与美国在政治关系走向融洽,同时高层交往不断、经济合作得到发展、军事交流恢复与加强,使印美关系得到改善与发展。美国与印度在后冷战时代都把对方看成是实现其战略目标的对象,这就是在后冷战时代美国与印度的关系不断改善与升温的动因。     

国有林场大苗移植成本核算初探

随着国有林场大苗移植工作的开展，使得大苗移植成本核算成为财务人员面对的新课题。通过对国有林场林木资产核算的现状分析，指出大苗移植培育成本核算可以采取的不同方法，并对相关业务的会计处理进行了探讨和研究。     

Tectonic types and evolution of Ordovician proto-type basins in the Tarim region

The Ordovician system is an important target for exploration in the Tarim Basin. Restoration of the Ordovician tectono-depositional environment is a key basis for the study of the structural development history in Tarim block and the prediction of the favorable Ordovician reservoir belts （zones）. Based on the surrounding tectonic settings, the litho-facies and sedimentary fill, the palaeo-geography, palaeoclimate and palaeo-ecology, and the structural deformation and magmatic eruptions, in this paper we combine the sedimentary fill in the basin with the development of the surrounding orogenic belts and re-build the proto-type basins of the different Ordovician periods. During the Ordovician period, the Tarim region was characterized by the composite of the interior cratonic depression with the peripheral cratonic depression. The interior cratonic depression in the central and western parts is mainly the deposiUonal area of the platform facies while the peripheral cratonic depression in the eastern part is mainly the zone of deepwater basin facies, with the slope acting as the transition belt between them. During the Late Ordovician period, the closure of the Northern Kunlun Ocean and destruction of the trench-arc-basin system in the Altyn Tagh region put the southern part of the Tarim block under com- pression and uplifting and turned the central and western parts of the carbonate platform into the mixed deposiUonal continental shelf. The eastern region of the basin had the over-compensated flysch sedimentation with huge thickness, marking the drastic turn of the basin nature. The basin tectonic framework turned to the south-north differentiation of the Silurian period from the east-west differentiation of the Ordovician period.