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   黄红色 的翻译结果: 查询用时:0.165秒
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黄红色
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  “黄红色”译为未确定词的双语例句
     The flesh is red-yellow in color with tiny brown spot,and taste sweet and crisp. Contents of soluble solids,vitamin C and soluble tannin are 16% to 18%,120 mg per 100 g of flesh and 0.032%,respectively.
     果肉黄红色,褐斑细小而少或无,肉质甜脆、爽口,果实成熟时可溶性固形物含量16%~18%,维生素C含量超过120mg/100g,可溶性单宁含量为0.032%,在树上完全自然脱涩。
短句来源
     Yellow-red coloring on aluminum and its alloy
     铝及铝合金化学着黄红色探讨
短句来源
     The colour characteristics of binary Pd-In alloys with different In contents were measured by Munsell and CIE colorimetric systems. The dependences of chromaticity of the alloys on the annealing temperatures were studied. It was found that the Pd-In alloys containing 36~60wt% In show yellow or yellow-red.
     用孟塞尔颜色系统和CIE 色度学系统研究不同In 含量的Pd - In 合金的颜色变化及退火温度的影响, 发现含36 % ~60 % (wt% 下同) In 的Pd - In 合金呈黄色或黄红色
短句来源
     Results: Compared with Vita Classical shade guide, Vita 3D Master extended itscolor in a* ,b*, which include more yellow-reddish and more saturate color tabs.
     结果:与Vita Classical比色板相比,Vita 3D Master比色片明度值在较低的区域也有分布,a*增大,使颜色向黄红色调方向移动; b*也增大,使颜色的饱和度增大。
短句来源
     postoperative vaginal discharge were reported in 0 to more than 40 days.
     术后阴道排黄红色液体持续(0~40多)天。
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  相似匹配句对
     Yellow-red coloring on aluminum and its alloy
     铝及铝合金化学着红色探讨
短句来源
     Seeing red
     “红色”柴油
短句来源
     THE RED VIOLIN
     红色重负
短句来源
     The Yellow Paint
     油漆
短句来源
     postoperative vaginal discharge were reported in 0 to more than 40 days.
     术后阴道排红色液体持续(0~40多)天。
短句来源
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Some wood properties of Eucalyptus exserta, E. citriodora and three hybrids planted in Leizhou peninsula were tested and the wood properties of E. citriodora proved the best.

经测定,雷州半岛的柠檬桉、窿缘桉及三种杂交桉的材性,以柠檬桉为最好。 测定了窿缘桉萌生和实生两种起源、两种杂交桉的三种类型(凸盘、凹盘及平盘)以及窿缘桉植生于其上的砖红壤性红色土和砖红壤黄红色土两种土壤类型等因子对材性的影响。就纤维长度、基本密度及生材顺压强度行进方差分析,初步结果表明;窿缘桉的两种起源之间及两种杂交桉的三个类型之间,材性均没有显著差异,生长在砖红壤性红色土的两种起源的窿缘桉的材性都优于生长在砖红壤黄红色土上者,虽然实生树的基本密度及顺压强度没有达到统计上的显著性。

Four remote Sensing image forms appear in the Lop nur region: white colored background image, dark yellow-red mushroom-form image, ear-form image and winding belt-form image. The dark yellow-red mushroom-form image indicates old evaporites and the site of potassium deposit. Characterized by its shallow depth it can be prognosticated that there will be more than 100 million tons of potassium chloride in this region.

新疆罗布泊地区的陆地卫星常规假彩色合成图像上有明显的四种不同影像区:白色背景影像区、暗黄红色蘑菇状影像区、耳朵状影像区和弯曲状条带影像区。笔者经分析研究认为,暗黄红色蘑菇状影像是古湖泊干涸区,为钾矿产地,钾盐品位高、埋藏浅,推测储量在1亿吨以上。

For the first time the surficial Quaternary deposits in the Huirou axea. Beijing, are divided from older to younger into the following five stratigraphic units; Middle Pleistocene, Upper Pleistocene, Lower Holocene, Middle Holocene and Upper Holocene. (1) The Middle Pleistocene: it consists mainly of slope-wash and diluvial deposits, 8 m thick; its lower part is marked by alternating beds of light red breccias and mild clays, while its upper part red and yellowish red angular fragment-bearing mild clays. (2)...

For the first time the surficial Quaternary deposits in the Huirou axea. Beijing, are divided from older to younger into the following five stratigraphic units; Middle Pleistocene, Upper Pleistocene, Lower Holocene, Middle Holocene and Upper Holocene. (1) The Middle Pleistocene: it consists mainly of slope-wash and diluvial deposits, 8 m thick; its lower part is marked by alternating beds of light red breccias and mild clays, while its upper part red and yellowish red angular fragment-bearing mild clays. (2) The Upper Pleistocene: its lower part consists of diluvial gravels with mild clays, 11.8 m thick, with thermoluminescent ages of 71±3.6 Ka and 66± 3.2 Ka;its middle and uppei parts are made up of alluvial mild clays and fine sands with several peat beds, 8.9 m thick, yielding mollusk fossils, with a thermolu minescent age of 27±1.4 Ka and C~(14) ages of 19.3-15.4Ka. The Holocene may be divided into three paits. (3)The Lower Holocene: it is composed of alluvial fine sands with gravels, 4-6 m thick, and locally represented by sandy clays and clays, 2 m thick, in which the peat interbeds were measured to have C~(14) ages of 9.291±0.161 Ka and 6.750±0.128 Ka. (4) Middle Holocene: it is marked by mild clays in the upper, black peat beds in the middle and fine sands and gravels in the lower, 5.1m thick, with C~(14) ages of 4.730-2.976 Ka. (5)The Upper Holocone consists of alluvial fine sands and gravels, varying in thickness from place to place, having a C~(14) age of 8.64±0.131 Ka.

作者首次将怀柔地区第四纪地层,由老至新划分成五个地层单位。中更新统为坡、洪积物,下部浅红色角砾岩与亚粘土互层,上部红、黄红色含角砾亚粘土,厚8m。上更新统下部为洪积砾石层夹亚粘土,厚11.8m,测得热释光年龄7.1±0.36万年,6.6±0.32万年;中上部为冲积亚粘土及细砂层,夹泥炭数层,厚8.9m,含软体化石,并测得热释光年龄2.7±0.14万年,C~(14)年龄1.93、1.72、1.54万年。全新统划分为以下三部分:下全新统为冲积细砂夹砂砾层,厚4.6m。局部为亚砂土及砂土层,厚2m,其泥炭夹层测得C~(14)年龄9291±161年及6750±128年。中全新统为冲积物,上部亚粘土,中部黑色泥炭层,下部细砂及砂砾层,厚5.1m;测得C~(14)年龄为4730—2976年。上全新统为冲积细砂、砂砾层,各地厚度不等,测得C~(14)年龄为804±131年。在1∶5万怀柔幅测区内,除西北隅有少量的低山丘陵外,近百分之九十的面积为第四纪堆积平原。由于该区第四纪以来主要以沉降为主,故地表所出露的第四系主要为更新统中晚期地层。现对其划分和对比情况介绍如下。

 
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