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逐渐变化

与 逐渐变化 相关的网络例句 [注:此内容来源于网络,仅供参考]

The trends of in-house and chemical composition that analysis of data of result dactylogram a collection of illustrative plates shows to different growth period is spent changes the pattern with definite existence, glucoside of foregone skin of bases peak shaddock accumulates peak period with thanking florescence to be, increase gradually as beautiful growth, when the flower dies of old age to form young fruit however drop off, show the regular; that after be being added first, decreases and peak area of glucoside of wild lacquer tree agrees basically, without apparent change.

结果指纹图谱数据分析显示不同生长期花的内部化学成分动态变化存在一定的规律,已知的主要成分峰柚皮苷以谢花期为积累高峰时期,随着花的生长逐渐增加,当花凋谢到形成幼果时却逐渐减少,表现出先增后减的规律;而野漆树苷峰面积基本一致,无明显变化。

Seed was stored in a storage temperature, the galactose content of seed decreases as the seed moisture content decrease. However, the glucose, fructose, sucrose and raffinose content of seed increase as the seed moisture content decreases, but this kind of change is not clear if seed was stored at lower temperatures ranges from 20℃ to -18℃.

然而葡萄糖、果糖、蔗糖和密三糖的结果与半乳糖的变化趋势相反,随着贮存温度的升高,四种糖的含量逐渐下降,在同一贮藏温度条件下,随含水量的降低,这四种糖的含量却逐渐升高,但在贮存温度较低时(20℃和-18℃),这种变化趋势不明显。

The plane interval changes are discussed in three situations: interval increasing, interval decreasing, interval changing according to sine curve.

将飞机间距变化情况分为间距逐渐增大、间距逐渐减小、间距呈正弦曲线规律变化3种情况讨论。

The analysis of TOC andδ13Corg benefits from Well Chao-73, indicating that they response well enough to the Cretaceous paleoenvironment and paleoclimate. During the sedimentary period of Quantou formation to Qingshankou formation in Songliao basin, the water tends to rise and becomes anoxic, and the deoxidized water leads to the organic matter massively preserved. The paleoclimate changes from torridity and aridity to warmth and humidity, with the temperature evidently descengded, then ascended in a litter range. The result is basically consistent with paleoclimate by the palynological analysis.

朝73井TOC、δ13Corg有机地球化学指标的分析结果表明,TOC、δ13Corg的变化对该沉积时期的古环境、古气候也有很好的响应,该沉积期湖水位不断上升,湖生生物逐渐发展并繁盛起来,水体含氧量减少,湖底有机质的保存环境逐渐变为强还原环境,大量有机质被埋藏并保存,而古气候在泉头组/青山口组界线上下由炎热干旱变得温暖湿润,气温有明显下降,但随后又有小幅的上升,与孢粉分析的古气候变化特征基本一致。

The thickness of the ice cover on the wall surface heat transfer is greater than the thickness of it on the air heat transfer form. The thickness of the ice cover on the wall surface heat transfer along the way changes slowly, but it on the air heat transfer along the way changes significantly. Reducing the entrance velocity, lowering the wall surface or air temperature, the formation of the thickness of the ice cover will increase; in the 3D circumstances, The thickness of the ice cover was relatively uniform in the import of the U-turn model, the ice cover was gradual accumulation in the convex bank when the stream traversed the import of the U-turn model, the thickness of the ice cover in the convex bank was significantly bigger than the thickness in the concave bank. The temperature field under the ice cover tends to be complex because of the existence of the secondary flows. The temperature in the convex bank is greater than it in the concave bank. Compared with the data from experiments, the laws in the numerical simulation are similar with them in the experiments

模拟结果显示:二维情况下,运用壁面传热形成的冰盖厚度大于运用空气传热形成的冰盖厚度,壁面传热形成的冰盖厚度沿程变化缓慢,而空气传热形成的冰盖厚度沿程变化明显,减小入口流速,降低壁面或空气温度等,形成冰盖的厚度都会增大;三维情况下,弯道入口处凸、凹岸形成的冰盖厚度基本相同,进入弯道后,凸岸形成的冰盖厚度逐渐增大,而凹岸的冰盖厚度逐渐减小,受横向环流的影响,冰盖下水流的温度场趋向复杂,并且凸岸的温度小于凹岸的温度;与实验室实验所得数据相比较,数值模拟研究得到的规律基本符合实验规律。

During thawing period, its soil water changes as season changes (the dynamic rule of soil water has the important relation of the season): from June to July the quality-moisture content of soil water gradually increases and reaches the highest, and from July to August it begins to decreases. The range of the quality-moisture content of the ground litter and humus layer is lower than the illuvial horizon whose quality-moisture content is gradually increasing in this thawing season.

在土壤冻土融化期,草类落叶松林土壤水分存在明显的季节性变化,土壤枯枝落叶层、腐殖质层质量含水量比淀积层质量含水量变化幅度大;6~7月份土壤含水量逐渐增加,达到最高;8月份以后土壤含水量开始降低;土壤淀积层质量含水量保持逐渐上升趋势;坡顶土壤质量含水量明显小于坡底土壤质量含水量。

The experimental results are as follows:(1) Without EAF the fouling resistance increase along with addition of time and change of the heat transfer coefficient is just contrary to the result. However, with EAF fouling resistance still enhances at the beginning of experiment and later, it gradually minishes after experiment has started for some time. Of course, the change of heat transfer coefficient still is contrary to the outcome. But when experiment lasts longer time, fouling resistance and heat transfer coefficient change in the same trend as the fore results at the beginning of the experiment. However, They all go to the tranquilization until the last.

实验结果表明:(1)没有经过电磁处理时,污垢热阻随着时间的增加而增加,换热系数随着时间的增加而减小;一旦经过电磁场的处理,污垢热阻开始时仍呈上升趋势,经过一段时间以后,便逐渐下降,换热系数的变化与此正好相反,即在实验开始时呈下降趋势,后来逐渐上升;当实验时间延长时,发现污垢热阻及换热系数在实验开始时的变化趋势与前面的实验结果基本相同,但到后来,二者的数值则分别均趋于稳定。

ANP and CX43 began to express at 2nd week after induction and increased gradually,about 60% of the resulting myogenic cells were positive at 4th week after induction ,they were negative for uninduced cells.hMSCs'surface antigen profiles obtained by Flow Cytometry were negative for CD31\CD34\CD45 before and after induction,but CD90 expressed higher after induction while was weak positive before induction(P.05). Apotosis index was correlated with the cultural time after induction,The apoptosis rate of induced hMSCs was remarkably higher than control group(P.01),and the variation between groups was notable(P.05),the cell cycle analysis showed that the percentages of G_0/G_1phases were reduced significantly after induction. The expresstion levels ofβ-MHC and CTNT mRNA were undetectable before induction,began to increase at 1st、4th week after induction,reached the peak at 6th week and decreased after that,the expression of Bcl-2 and Bax mRNA varied regularly after treated with 5-azacytidine. hMSCs'resting membrane potential、range and rate of depolarization were heightened gradually after being induced.

结果:hMSCs诱导前为纺锤形,诱导后第2天部分细胞即开始发生形变,呈球形或短棒状,1周后胞浆中颗粒增多,约20~30%细胞边缘呈毛刷样变化;hMSCs表面抗原CD31、CD34、CD45在诱导前后差异无统计学意义,CD90未诱导时表达呈弱阳性,诱导后明显增高(P.05);ANP和CX43在诱导前无表达,诱导后第2周开始表达且表达随时间逐渐增强,但CX43在诱导后第5周表达量开始降低。hMSCs诱导后凋亡指数随诱导后培养时间增加,低浓度诱导组低于标准浓度诱导组,组间差异有统计学意义(P.05),G_0/G_1期细胞比例诱导后较对照组显著减少(P.05);β-MHC和CTNT基因分别在诱导后第1周和第4周时表达开始增强,在第6周时均达到高峰,第8周时表达开始衰减,Bcl-2、Bax基因表达呈时间依赖性变化,hMSCs经诱导后随心肌样细胞特征的表达膜静息电位、去极化幅值和去极化速率逐渐增高。

Results showed that the overland flow pattern has close relationship with the grass cover and water inflow rate, it changed from the laminar and tranquil flow to the transition flow and tranquil flow for the grass-covered sloping segment with increasing water inflow rate, but it was almost transition flow and tranquil or rapid flow for the sloping segment without grass cover.

结果表明,坡面流流态与放水流量和草被覆盖关系密切,随流量的增大草被覆盖断面坡面流流态由层流-缓流转变为过渡流-缓流,而无草覆盖断面的流态几乎都处于过渡流-缓流或急流状态;沟坡径流大都属于过渡流-急流状态,试验过程中,草被覆盖断面的径流雷诺数和弗汝德数变化很小,无草被覆盖断面径流的雷诺数呈逐渐增加趋势,而弗汝德数呈逐渐减小的变化趋势。

are gained that after widening, the settlement of two sides of the old road pavement is contrary, cross slope of old road is different, horizontal displacement of the old road pavement is minishes, the area of maxium settlement, maxium lateral displace and disease of old road is different as before widening.

分析结果指出:在拓宽段作用下,靠近老路中心一侧老路路面沉降逐渐减小,远离老路中心一侧沉降逐渐增大,相应横坡也在发生变化;老路路面的水平位移有较大幅度的减小;而且老路最大沉降、最大水平位移、最大剪应力及最易发生病害的位置与拓宽前也发生了较大的变化。

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