低温胁迫下钼对冬小麦光合作用特性的影响

研究了低温胁迫下施钼对冬小麦钼高效品系97003和钼低效品系97014叶片光合参数的影响。结果表明，低温胁迫下施钼显著提高2个品系叶片的净光合速率(P_n)和气孔限制值(L_s)，显著降低叶片气孔导度(G_s)、胞间CO₂浓度(C_i)和蒸腾速率(T_r)。随着低温处理时间的延     

玉米超氧物歧化酶酶谱型的遗传分析

我们在吉林省主要玉米自交系中曾发现两种超氧物歧化酶变异型。1988年采用酶谱型不同的3个自交系配制了2个杂交组合。根据F1、F2和F3的资料对玉米超氧物歧化酶酶谱型的遗传方式进行了分析。结果表明，玉米超氧物歧化酶SODala2的有无受一对主效基因控制，以Sod1和sod1表示。     

山茱萸总黄酮提取工艺的研究

以乙醇为提取溶剂,用温浸法从山茱萸中提取总黄酮,并通过单因素考察和正交试验优化工艺条件.结果表明,在优化工艺浓度为40%、料液比1:15、温度为70℃的水浴中25 h的工艺条件下,总黄酮的得率为8.61%.     

几种化学物质和温度处理对高羊茅种子发芽的影响

用高羊茅(Festuca arundinacea)种子为试验材料,置入光照培养箱培养,研究化学物质和温度处理对其发芽的影响.结果表明:0.2%的次氯酸钠(NaClO)处理促进高羊茅种子的发芽,浓度梯度设置在0.5%～1.5%时均抑制其发芽,且浓度与发芽率和发芽势均成负相关.不同浓度的硝酸钾(KNO3)处理均促进其发芽,且浓度为2.0%时,发芽率最高,发芽势是先降低后升高.高羊茅最适播种温度为20℃,高于或低于20℃,对种子的发芽均有不同程度的抑制作用.     

两段发醇法酿制酱油

食盐在发酵繁殖中能防止杂菌的繁殖,所以采用传统方法酿制酱油要加食盐水发酵,但食盐对酶活性有抑制作用,随着食盐浓度的增加,相对地延长了发酵周期.采用两段发酵法酿制酱油即可取得事半功倍的作用.……     

地面数字图像技术在棉花氮素营养诊断中的初步研究

为了探讨利用图像处理技术进行棉花氮素营养诊断的可行性,通过多水平的氮肥田间试验,采用数码相机获取棉花冠层图像,分析了不同氮水平下棉花冠层图像色彩参数与施氮量、产量及多个氮素营养诊断指标之间的关系.研究表明:南疆畦灌条件下,氮素营养水平直接影响到棉花冠层光谱反射特性.红、蓝光标准化值与铃期施氮量、产量之间有极显著的线性负相关关系,采用R/(R G B)、B/(R G B)值可以直接用来诊断棉花铃期的氮素营养状况,或间接估测产量;铃期绿光值G和绿光与红光比值G/R与叶柄硝酸盐浓度、植株全氮和地上部生物量之间都有较大的相关性,可以较为灵敏地反映棉花氮素营养水平,适宜作为氮素营养诊断指标.因此,应用数字图像技术进行棉花氮素营养诊断是可行的.     

间作大豆喷施增产灵和TIBA的效应

本文试验用增产灵和２，３，５－三碘苯甲酸（ＴＩＢＡ）对间作大豆不同生态类型品种进行喷施。喷施增产灵后，对早熟矮杆品种各处理均表现增产，其增产幅度为０．３７％－６．７５％，施用时期以结荚期为佳；早中熟、中杆、生长较为繁茂的品种仅在开花期喷３０ｐｐｍ可增产１２．０６％；增产灵的增产作用主要是由于提高了单株叶面积、叶绿素含量、单株粒重和百粒重。喷ＴＩＢＡ后，对植株主要起降矮壮杆的作用，株高降矮０．５２－１０．７８ｃｍ，抗倒能力增强，早熟、矮杆的７５－８８－１３开花期喷施呈减产效应，而结荚期喷施可增产０．４７％－３．５％；早中熟、中杆的冬二则在开花期喷施可增产６．４２％．     

二级缓释熏蒸在六面密闭粮堆中的应用

通过对六面密闭麻袋包装小麦粮堆分别采用二级缓释熏蒸、常缓熏蒸和缓释熏蒸的施药方法进行对比试验。结果表明,采用二级缓释熏蒸保持PH3有效浓度时间最长、Ct值最大,熏蒸效果最理想。采用5.3 g/m剂量,全年只熏蒸1次即可保持粮堆全年无害虫。     

高大平房仓PVC管膜下环流熏蒸试验

高大平房仓密闭粮堆上层增设PVC管通风网络，进行PH3环流熏蒸实验。按1．5g／m^3计算AlP用药量，通风笼投药后环流72小时，粮堆内PH3浓度达到均匀分布，粮堆最高浓度值达到396mL／m^3，且有效浓度保持了30天，杀虫效果达100％。     

用树轮δ13C重建过去300年大气CO2浓度

The annual series of δ13C were measured in tree rings of three Cryptomeria fortunei disks （OF-1, OF-2, and OF- 3） collected from West Tianmu Mountain, Zhejiang Province, China, according to cross-dating tree ring ages. There was no obvious decreasing trend of the δ13C annual time series of CF-2 before 1835. However, from 1835 to 1982 the three tree ring δ13C annual series exhibited similar decreasing trends that were significantly （P ≤ 0.001） correlated. The distribution characteristics of a scatter diagram between estimated δ13C series of CF-2 from modeling and the atmospheric CO2 concentration extracted from the Law Dome ice core from 1840 to 1978 were analyzed and a curvilinear regression equation for reconstructing atmospheric CO2 concentration was established with R2 = 0.98. Also, a test of independent samples indicated that between 1685 and 1839 the reconstructed atmospheric CO2 concentration .using the δ13C series of CF-2 had a close relationship with the Law Dome and Siple ice cores, with a standard deviation of 1.98. The general increasing trend of the reconstructed atmospheric CO2 concentration closely reflected the 10ng-term variation of atmospheric CO2 concentration recorded both before and after the Industrial Revolution. Between 1685 and 1840 the evaluated atmospheric CO2 concentration was stable, but after 1840 it exhibited a rapid increase. Given a longer δ13C annual time series of tree rings, it was feasible to rebuild a representative time series to describe the atmospheric CO2 concentration for an earlier period and for years that were not in the ice core record.