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笋生长
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  “笋生长”译为未确定词的双语例句
     SHOOTING AND GROWTH OF BASHANIA FARGESII
     巴山木竹发笋生长规律的观察
短句来源
     Influence of Leaf Fertilization on Phyllostachys Shoot Grown from Seed
     叶面施肥对实生毛竹苗鞭笋生长与萌发的影响
短句来源
     Primary Study of Nutrients and Law of Growth and Development Disun(Lycopus lucidus Turcz)
     地笋生长发育规律及营养成分的初步研究
短句来源
     The process lasts about 70 days. Regression equation could forecast the growing process well. The amount of growing during the day(58.13%) is larger than that of during the night.
     前期不同时间出土的笋,其高生长停止的时间基本相同,需时约70 天,白天的高生长量(58.13%)大于夜晚的,回归模型能很好地预测笋生长过程;
短句来源
     Through comparison and comprehensive analysis of five carrot cultivars,it was showed that the Japanese carrot cultivar Sanhongjinsun was with stronger growth ability,vigorous plant,long and round taper shaped root,238.27g of average weight per root,straighter root,smooth surface,less root diameter difference between the top and bosom of mature root,external,middle and internal layers of root was turkey red,thin xylex and deep phloem,higher contents of soluble solid matter,vitamin C and carotene,and high quality.
     通过对5个胡萝卜品种的比较及综合分析,认为日本三红金笋生长势比较强,植株生长健壮,肉质根为长圆锥形,平均单根重238.27 g,较直,表面光滑,成熟根茎上下粗度较为一致,肉质根外、中、内三层均为鲜红色,心柱细小,肉质肥厚;
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  相似匹配句对
     Rule of Shooting and Height growth of Dendrocalamus latiflorus
     麻竹出和高生长规律的研究
短句来源
     SHOOTING AND GROWTH OF BASHANIA FARGESII
     巴山木竹发生长规律的观察
短句来源
     growth of diameter ,height and volume;
     材积生长
短句来源
     Growth of Order
     秩序的生长
短句来源
     STUDIES ON THE VINIFICATION OF BAMBOO SHOOTS EXTRACTS
     汁酿酒的研究
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Neosinocalamus affinis is a bamboo species distributed most widely and cultivated for a long time. The following problems about it is discussed in this paper.1) The growth of the bamboo species under various stand conditions shows that there is no significant correlation between the density of the clump of the bamboo and the stand conditions, that the density is limited mainly by the thickness of soil, and that the height and the breast-height diameter of the bamboo correlate with the altitude above sea level.2)...

Neosinocalamus affinis is a bamboo species distributed most widely and cultivated for a long time. The following problems about it is discussed in this paper.1) The growth of the bamboo species under various stand conditions shows that there is no significant correlation between the density of the clump of the bamboo and the stand conditions, that the density is limited mainly by the thickness of soil, and that the height and the breast-height diameter of the bamboo correlate with the altitude above sea level.2) It is shown that the diameter and the height of the bamboo and its clump density decrease with the decrease in thickness and humidity of the soil from the valley to the top of the slope when the series of the bamboo in the valley is investigated.3) Study on the growth and development of the bamboo shoots shows that the increment of the bamboo correlate mainly with yesterday's humidity and today's temperature. The growth curve exhibits tow peaks for one day; the first is before 10 a.m., the second is after 3 p.m.. The number of the bamboo shoots which appeared above the ground correlate with the thickness of soil, whereas the number of the bamboo shoots which disappeared above the ground is mainly limited by the height of the mother bamboo and the number of the bamboo shoots which appeared above the ground. The number of healthy bamboo shoots is mainly affected by the thickness of soil and the bamboo height.

慈竹生态研究的结果如下: (1)用逐步回归分析模型分析,慈竹竹丛密度仅与土壤厚度关系密切。慈竹高度、胸径与海拔成正相关。(2)用逐步回归法分析笋生长量与气候因子间的关系,证明笋的逐日生长量与湿度,温度和降雨量有较密切关系,笋在一天内有两个生长高峰。(3)自然条件下,出笋数主要与土厚密切相关,退笋数受母竹高和出笋数所制约,好笋数主要受土厚和竹高影响。

The reason why δ18O Curve of deep Sea sediments and some living thing's Crusts successfully reflects the change of paleotemperature is reviewed in this paper.Then, thedifficulty of study on paleotemperature under the environment of land is discussed. The progress of Paleotemperature of spele-othems in Cave can be divided in to 3 stages:determining property, semi - determining amounts,determining amounts. At last, theauthor discuss the three factors infecting paleotemperature's reliability of speleothems in cave....

The reason why δ18O Curve of deep Sea sediments and some living thing's Crusts successfully reflects the change of paleotemperature is reviewed in this paper.Then, thedifficulty of study on paleotemperature under the environment of land is discussed. The progress of Paleotemperature of spele-othems in Cave can be divided in to 3 stages:determining property, semi - determining amounts,determining amounts. At last, theauthor discuss the three factors infecting paleotemperature's reliability of speleothems in cave.

本文回顾了深海氧同位素曲线成功地反映了古温度变化的原因,分析了陆相环境古温度定量研究的困所在.洞穴钟乳石古温度研究经历了定性、半定量和定量三个发展阶段.最后对古温度定量研究中的三个影响因素(水的δ18O,石笋生长速率及同位素分析精度)进行了探讨.

Applying the isotopic dating and temperature-probing techniques,the isotopic pale-otemperature of the speleothems evolutions from the Tian-e Cave,Ninghua county of Fu-jian Province,is obtained based on the O' Neil' s Equation. The temperature evolutionalcurve is compared with that of the global O isotopic curve of deep-sea foraminifera ,whichshows that:in this area there had obviously experienced five times of large temperaturevariation processes from about 210 ka to 18 ka BP,which corespond to the 6th,the...

Applying the isotopic dating and temperature-probing techniques,the isotopic pale-otemperature of the speleothems evolutions from the Tian-e Cave,Ninghua county of Fu-jian Province,is obtained based on the O' Neil' s Equation. The temperature evolutionalcurve is compared with that of the global O isotopic curve of deep-sea foraminifera ,whichshows that:in this area there had obviously experienced five times of large temperaturevariation processes from about 210 ka to 18 ka BP,which corespond to the 6th,the 5th,the4th,the 3rd and the 2th stage respectively in the oxygen isotopic periodity. It is estimatedthat the Riss glacial ended up at about 155 ka BP,and the Wurm subinterglacial began atabout 65 ka BP, Results argue that there was no conditions to form glacier in this area un- der the Late Quaternary paleoclimate environments, which was influenced by the globaltemperature variations substantially.

应用同位素地球化学方法,并以现代溶岩水的δ ̄18O_w代替石笋生长时期原生包体水的δ ̄18O_w,根据O’Neil方程,计算了福建宁化天鹅洞内第四纪碳酸盐堆积物的古温度。结果表明,温度计算偏差在±0.5℃左右。在与全球深海氧同位素曲线对比后,指出该地区大约在210~18kaBP,武木亚间冰期的起始时间(氧同位素期3/4阶界限)估计在65kaBP。结果表明,福建宁化地区晚第四纪古气候环境没有形成冰川的条件,但明显受到全球气温变化的控制。

 
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