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The results showed the content of GA3 and IAA first increased and then decreased,and ABA gradually increased with dehydration ratio in leaves of Citrange and Shanxiahong.But the change of Z content was different between Citrange and Shanxiahong.

结果表明:经不同程度干旱处理的枳橙叶片GA3I、AA、Z含量都呈先升后降的变化趋势,ABA含量随着失水率的增加逐渐上升;而山下红叶片GA3I、AA含量都呈先上升后下降的变化趋势,Z含量变化有些起伏,ABA含量随着失水率的增加逐渐上升。

The results showed the content of GA3 and IAA first increased and then decreased, and ABA gradually increased with dehydration ratio in leaves of Citrange and Shanxiahong. But the change of Z content was different between Citrange and Shanxiahong. The content of Z first increased and then decreased in Citrange, but waved in Shanxiahong.

结果表明:经不同程度干旱处理的枳橙叶片GA3、IAA、Z含量都呈先升后降的变化趋势,ABA含量随着失水率的增加逐渐上升;而山下红叶片GA3、IAA含量都呈先上升后下降的变化趋势,Z含量变化有些起伏,ABA含量随着失水率的增加逐渐上升。

The numerical results indicated that the mixing time decreases about linearly with increasing current intensity. The mixing time decreases first then increases with increasing current frequency and comes up to its minimum value at 30Hz. Applying the traveling magnetic field to the uptake or downtake when the exciting current intensity is 200 A at 10 Hz, the mixing time can be shortened by 9%~17%. With the operating conditions kept unchanged, shorter mixing time is available if applying the traveling magnetic field to the uptake instead of downtake, and the time can be shortened by 18%~26% if applying the magnetic field to both the uptake and downtake. Moreover, the mixing time decreases with increasing argon blowing flowrate, and the time comes down to its minimum value if the argon blowing flowrate is 1 600 NL/min. After the moment, the mixing time increases with argon blowing flowrate.

计算结果表明:混匀时间随电流强度的增大而减小,并且近似成线性关系;混匀时间随电流频率的增加先减小后增大,并且在30Hz 时达到极小值;在励磁电流强度为200A ,频率为10Hz 的条件下,在上升管或下降管施加行波磁场混匀时间可缩短9%~17%;在相同操作条件下,在上升管处施加行波磁场混匀时间小于在下降管施加行波磁场的混匀时间;同时在上升管和下降管施加行波磁场,混匀时间可缩短18%~26%;混匀时间随吹氩量的增大而减小,在吹氩量为1600NL/min 时混匀时间达到极小值,吹氩量继续增大时,混匀时间反而增大。

The result of experiment shows that the hardness will increase and the plating rate will decrease with the rising of concentration ratio of nickel sulfate and hypophosphite.

最后的试验结果表明,在其它条件不变的情况下,随着镍磷摩尔浓度比的增大,镀层硬度逐渐上升,而镀速逐渐下降;在其它条件不变的情况下,随着丙酸浓度的增加,平均镀速有所上升,而硬度先上升,达到一个最大值后开始下降。

From thermal analysis, weight loss occurs pronouncedly at temperatures above 300 oC in air and the residual weight increases with the reaction temperature. The particle size decreases with the increasing ethanol concentration., while the BET surface area decreases when the concentration of water is increased. Pore size measured from the as-synthesized particles is about 2.7 - 4 nm and this becomes slightly smaller after calcination which is about 3 - 5 nm.

TG/DTA中温度上升至约300 oC时,重量开始明显失重,随著合成反应温度上升,最终残留量由1~3%提高为约5~7%,动态光散射粒径分析发现随著乙醇含量增加,煅烧前与煅烧后的粒径尺寸均有下降趋势,随著水含量的增加,比表面积值随著下降,煅烧后的壳层孔隙尺寸约为3~5nm,煅烧前的壳层孔隙尺寸为2.7~4 nm,煅烧后的孔隙度会略为上升。

The percent of Cosmopolitan genus increase along with the elevation, but the trend is contrary to that of the pteridophyte genus.

在垂直梯度上:种子植物属热带分布诸类的比例自海拔400至800米(~1100米)之间呈上升趋势,然后下降;温带分布的第8、9、10、11类随海拔而上升;地中海—中亚中心分布的第12、13类只见于比较干热的河谷地带;东亚分布和中国特有属在海拔900~1100m和1600~1800m段取得小的峰值;世界分布属的比例随海拔而上升,蕨类植物属则相反。

The results showed that different topping frequency (at intervals of 15 d, 30 d, 60 d, 90 d) had no evident influence on total wine loss, volatile acid content, T-SO2,F-SO2, wine colour, and wine pH values. Under constant temperature and humidity conditions, total wine loss was closely correlated with the using degree of Chinese barrel and the storage time in Chinese barrel. Volatile acid content slightly rose along with wine storage time. The content of SO2 dropped rapidly during 15 d after wine filling, but dropped tardily ever since. Wine colority rose remarkably during 15 d after wine filling, but climbed tardily ever since. Wine colority change was unstable, it changed wavily and depressed on the whole. In conclusion, it was recommended that the best topping interval was 90 d.

结果表明,橡木桶15 d、30 d、60 d、90 d添桶间隔对红葡萄酒的酒液损失总量、挥发酸含量、T-SO2、F-SO2、颜色、pH值无显著影响;在恒温恒湿的条件下,红葡萄酒的酒液损失总量与橡木桶的新旧程度、桶贮时间密切相关;随桶贮时间延长,葡萄酒中挥发酸略有上升;葡萄酒入桶后15 d内SO2含量急剧下降,以后则缓慢下降;葡萄酒入桶后15 d内色度显著上升,但随后变化平缓,总的趋势是随桶贮时间延长色度缓慢上升;葡萄酒的色调变化不稳定,呈波浪式变化,总的趋势是降低;建议中国橡木桶桶贮红葡萄酒的添桶间隔为90 d。

The P-C-T curves for Ti_(0.17)Zr_(0.08)V_(0.35)- Cr_(0.1)Ni_(0.3) and Ti_(0.17)Zr_(0.08)V_(0.35)Cr_(0.1)Ni_(0.3)Mm_(0.01) alloys have been depicted by electrochemical methods. It is shown that as temperature rises, the hydrogen equilibrium pressure of the alloys goes up, but the hydrogen desorbing performance deteriorates. After addition of Mm, the hydrogen equilibrium pressure of the alloy comes down, and the hydrogen desorbing performance meliorates.

同时本文还通过电化学方法绘制了Ti_(0.17)Zr_(0.08)V_(0.35)Cr_(0.1)Ni_(0.3)和Ti_(0.17)Zr_(0.08)V_(0.35)Cr_(0.1)Ni_(0.3)Mm_(0.01)合金的P-C-T曲线,发现,温度上升时,Ti_(0.17)Zr_(0.08)V_(0.35)Cr_(0.1)Ni_(0.3)合金的平衡氢压上升,随温度上升,合金的放氢特性变差;添加Mm后,合金的平衡氢压降低,曲线的整体斜率变小,放氢平台宽度增大,说明合金的放氢特性得到改善。

Schematizing the southern Yellow sea as an constant water depth and semi-enclosed rectangular bay, the evolution trends of tidal amphidromic system of M2and variation features of coast tidal range are analyzed primary under the condition of 3 and 5 meter rise of sea level respectively.

将南黄海概化为一等深矩形海域,初步研究了在海平面上升 3m 和 5m 条件下该海域旋转潮波系统的演化趋势,继而分析了沿岸潮差变化特征。初步分析研究表明:随着海平面上升,该海域 M2 分潮的无潮点有向东南方向偏移的趋势,受此影响,沿。。。应用海湾和半封闭矩形海域改进的 Taylor 问题的解研究海平面上升对 M2 分潮旋转潮波系统及沿岸潮差的变化。

Using maximum flooding surface and local explosure erosion surface as the correlation framework surface in the 4-th hierarchical base-level cycles, sand-body in the 3-th hierarchical base-level cycles formed in the 4-th hierarchical base-level cycles may be correlated layer by layer. The law of the sand-body and the characters of reservoir heterogeneity formed in the 4-th hierarchical base-level cycles are discussed. The study shows:①During early period of the 4-th hierarchical base-level cycle rising, subaqueous distributary channel formed, continuously stacked vertically, and migrated in limit range laterally, and channel sand-body stretches farther longitudinally, and lacks interbeds of mud rock and siltsand in sand rock, reservoir heterogeneity is relatively weak.②During mid-period of the 4-th hierarchical base-level cycle rising, subsaqueous distributary channel migrated actively, channel divided and converged strongly to form netted sand-body and sand sheet mainly, but interbeds of mud rock and siltsand increases gradually in sand-body, reservoir heterogeneity increased.③During later period of the 4-th hierarchical base-level rising and early period of the 4-th hierarchical base-level falling, reservoir sand-body was poor, and only form thin sand-body of subsaqueous distributary channel, subsaqeuous creveas and distal mouth bar, sand-bodys are surrounded by mud and silt rock.

进一步采用以第4层次基准面旋回中相当最大湖泛面的相转换面和具有区域性暴露侵蚀作用的层序边界面为等时地层对比框架的边界,对发育于MSC2—MSC4三个第4层次基准面旋回的第3层次基准面旋回内砂体进行了逐层等时对比,探讨第4层次等时地层对比格架内储集砂体发育分布规律,及储集砂体的非均质性特点,研究发现:①第4层次基准面上升初期发育的水下分流河道,砂体呈连续叠置、侧向迁移受限,纵向上呈长距离延伸的带状产出,砂体间泥、粉砂岩夹层少,储层非均质性相对较弱;②在第4层次基准面上升中期发育的水下分流河道侧向迁移活跃,纵向延伸过程中分流汇合作用强烈,以形成网状或席状连片砂体为主,但砂体间泥、粉砂岩夹层逐渐增多,储层非均质性增强;③第4层次基准面上升晚期和下降早期,不利于储集砂体发育,仅出现少量薄的水下分流河道、水下决口扇、远—河口砂坝砂体。

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