- 更多网络例句与垆相关的网络例句 [注：此内容来源于网络，仅供参考]
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The results show: the most sensitive Chinese area to acid deposition is Podzolic soil area, then follow Latosol, Dark brown forest soil and Black soil areas; Ferraisol and Yellow-brown earth area in southern China can buffer about 0.8-1. 6 g Sm〓yr〓 sulfur deposition; the least sensitive areas to acid deposition are mainly Xerosol area in northwest China, Alpine soil area in the Qingzang Plateau, and Dark loessial soil and Chernozem areas; the main reason for lower critical load in northeastern areas and higher critical load in Ferralsol and Yellow-brown earth areas in China can be attributed to the obvious difference in temperature, humidity and soil properties.
研究表明：我国土壤对酸沉降最敏感的区域是漂灰土带，其次是砖红壤土区、暗棕壤带和黑土区，南部富铝土区域大致可接受O.8-1.6 g Sm〓yr〓的硫沉降，对酸沉降最不敏感的区域主要集中在西北干旱土和青藏高原的高山土区域以及黑垆土和黑钙土带；导致我国东北地区酸沉降临界负荷偏低和富铝土区域酸沉降临界负荷偏高的重要原因，是这些地区的气温、湿度和土壤质地存在显著差异。
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This indicates that the soil under observation was clayey or loamy.
这说明所研究的土壤属亚粘土或垆坶土。
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The ship was completely buried in the soft loam of the sea bottom.
这条船被完全埋到海底松软的肥土里。3。垆姆，亚黏土
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The interval has been achieve at millenary- scale.
黑垆土地层的沉积速率不是均一的。
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Accumulation and distribution of available sulfur (0.15% CaCl2 extract) in the limy soil profile with a 15 year fertilization experiment were studied.
对设在黄土高原旱地黑垆土上不同N、P配比与用量的长期定位试验土壤剖面有效硫的分布与累积进行了研究。
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The dissociation constants p K HL1 is in the range of 3\^50 to 4.89, p K HL2 6.17 to 8.38, K HL1 / K HL2 is below 10 5, which is consistant with the results of potentiometric titration curve. The Cu 2+ complexation constant,is 1.346 for old manured loessal soil and 2.241 for dark cultivated loessal soil.A good optimization result is given by nonelectrostatic model.
胡敏酸的解离常数和Cu2+的络合常数应用计算机程序FTTEQL32表明，优化的解离常数pKHL1在3.50-4.89之间，pKHL2在6.17-8.38之间，2种形态一元胡敏酸解离常数之比小于105，与滴定曲线只有一个突跃区相一致2种土壤胡敏酸与Cu2+络合常数logKintACu大小分别为土HA1.346，黑垆土HA 2.241，非静电模式的优化结果较好。
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The results show that the2 0～ 40 cm and40～ 60 cm layers for the red loessial soil and2 0～ 40 cm layer for the red loessial soil had a large amount of easily mineralizable nitrogen besides the0～ 2 0 cm layer, but the easily mineralizable nitrogen was little...
总体上看，红油土中氮素的矿化和硝化作用强于红垆土。铵态氮肥在粘粒含量少、有机质含量高土层中的迅速减少主要归咎于硝化，而在粘粒含量多、有机质含量少的土层，主要取决于矿物固定
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In order to study the finger flow phenomenon during ponded infiltration process in layered soil, an experimental study was carried out to observe the occurrence, mechanism and environment of finger flow in six soil columns which have different grain sized sands overlain by loess soil.
根据层状结构土壤在积水入渗过程中存在发生指流的现象，该文针对黄土地区&垆盖砂&的土壤条件，在室内以西安黄土为主体，对6种不同粒径的砂质双层结构土壤进行积水入渗试验，以观测研究发生指流的现象、机理与条件。
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Then the author aims at the question on the image of Wenjun, four important parts we take of this paper: enters the stage, elopes, sells wine, the resentment recite as the clue, how different performance in different writers and compares with the image of history. Analyzes the characteristic Wenjun's image in the traditional opera.
然后笔者则针对文君形象的塑造问题，以文君在戏曲中的四大重要戏份——出场、私奔、当垆、怨吟为线索，分析在不同作家笔下女主角文君有着怎样不同的表现，并与《史记》中的文君形象比较，分析出古典戏曲中各具特色的文君形象。
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There are three effects that may be important in producing this trend. First, lowtemperature oxidation preferentially affects the finer single-domain magnetites responsible for the Hopkinson peak, which is therefore suppressed in the more oxidized loams. Second, the possible production of uniaxial magnetite with shape anisotropy can also lead to a relatively muted Hopkinson peak. There is, additionally, a third alternative, and the one preferred here, that the natural alteration processes involved in pedogenic susceptibility enhancement have probably depleted the supply of ironbearing precursor phases, so that less new magnetite is formed on heating.
产生这种特殊热磁性质的可能原因如下：第一，成土过程中的低温氧化作用减弱了磁铁矿的Hopkinson效应；第二，可能是成土过程中生成的一向延长的针状磁铁矿颗粒表现出较弱的Hopkinson效应；第三，随着成土作用增强，现代黄土、黑垆土中的硅酸盐、粘土矿物因受土壤化作用分解而越来越少，加热过程中分解产生的磁铁矿造成的磁化率增强相对于其初始磁化率也就越来越小，从而产生越来越弱的Hopkinson/alteration峰，本文认为这是最主要的原因。
- 更多网络解释与垆相关的网络解释 [注：此内容来源于网络，仅供参考]
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image broadening：象加宽
rolandometer 大脑皮质沟测定器 | image broadening 象加宽 | fine sandy loam 细砂壤土, 细亚砂土, 细砂质垆坶
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floodplain：河漫滩
[14] 河漫滩(floodplain) 当河流洪水泛滥时,除河床以外,谷底部分也被淹没,被淹的河底滩地称为河漫滩. [7] 褐土(cinnamon soil) 在旱生森林灌木丛草原下形成的,在水平分布上处于棕壤和黑垆土带,栗钙土带之间,在垂 直分布上出现在棕壤带之下.
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loadstone; lodestone：极磁铁矿;磁石
"负载沈降曲线","load-settlement curve" | "极磁铁矿;磁石","loadstone; lodestone" | "壤土;垆姆","loam"
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mantle plume：地幔涌流
盖层垆坶 mantle loam | 地幔涌流 mantle plume | 地图 map
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mellow soil：松软土壤,熟土
mellow loam 松壤土,松散垆坶 | mellow soil 松软土壤,熟土 | mellow tilth 耕耘土壤
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Dark loessial soils：黑垆土
灌淤土 Cumulated irrigated soils | 黑垆土 Dark loessial soils | 粗骨土 Skeletol
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Cumulated irrigated soils：灌淤土
寒钙土 Frigid calcic soils | 灌淤土 Cumulated irrigated soils | 黑垆土 Dark loessial soils
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clayed sugar：(白土脱色的)漂白蔗糖
claybank || 土堤, 棕黄色 | clayed sugar || (白土脱色的)漂白蔗糖 | clayey loam || 亚粘土, 粘土质垆坶