查询词典 turn up soil

Furthermore, the impact factor on runoff showed that, each stage has different impact factors, soil temperature and soil moisture above 65 cm plays a leading role in spring flood; in summer dry season, relation of soil temperature and moisture above 40 cm and runoff is negative correlation, the deeper soil temperature and soil moisture plays a leading role; temperature and precipitation plays a leading role in summer flood; in autumn dry season, the impact factors are soil temperature, soil moisture and temperature.

径流影响因子分析的结果表明：径流过程中不同时段具有不同的主导因子，春汛期主要是65cm以上的土壤温度和水分起主导作用；夏季枯水期40cm以上土壤水分与径流是负相关，深层地温和土壤水分起主导作用；夏汛期气温、降水起主导作用；秋季枯水期的影响因子依次为土壤温度、水分及气温。

By employing indicators as soil PH, conductance and salt content, different soil salinity degrees are plotted out. There arc 9 types of salinisation levels in Fukang oasis. Within them, the strong saline soil and solonchak are the main types, which, with regards to latitude and from the lower of diluvial fan to desert, distribute in turn as middle saline soil, strong saline soil, solonchak, strong saline soil, solonchak and non- saline distribute.

该文以电导、易溶性盐含量、pH作为盐渍化程度的指标，将阜康绿洲的土壤盐渍化程度划分为9种类型，其中以强盐渍土和盐土为主，在纬度梯度上从南至北，即从洪积扇下部到沙漠按照中盐渍土－强盐渍土－盐土－强盐渍土－盐土－非盐渍土的顺序依次分布。

Shanghai Impregnant Factory located in the Park of World Expo 2010 Shanghai was set up 70 years ago and abandoned for 10 years. The quantities of soil microorganisms, soil enzyme activities, soil chemical properties and their relationships under Cinnamomum camphora community, Metasequoia lyptostroboides community, Nerium indicum community and Cinnamomum camphora+Ligustrum lucidum shrub community in the factory were studied. Results showed that the differences in soil properties were significant in upper soil layer (0~20 cm) and the vertical distribution rules of soil properties were different under four plant communities.

对2010年上海世界博览会规划园区内，已废弃的上海市溶剂厂的绿地低干扰下的香樟群落、水杉群落、夹竹桃群落、香樟和女贞灌丛群落的土壤微生物数量、土壤酶活性及土壤化学性质等特性及其关系进行分析。

Eagles--Last Good Time In Town [00:20.02]1223_dd制作 [00:58.45]I like to go out every now and then [01:02.30]I can't wait to do it again [01:06.19]But I haven't had the time [01:10.81]Lately [01:14.27]I like to step out every once in a while [01:18.89]I kind of like to do it in style [01:22.90]I haven't had the time [01:26.96]Lately [01:31.70]Lately I've been stayin' at home [01:35.60](Stayin' at home, stayin' at home) [01:39.73]Workin' the crosswords, turn off the phone [01:43.85](Turn off the phone, turn off the phone) [01:51.71]And I dream I'm on vacation [01:55.86]'Cause I like the way that sounds [01:59.98]It's a perfect occupation [02:04.27]For me [02:08.90]I don't mind being by myself [02:12.72]If there's no one else around [02:16.69]It's the last good time in town [02:38.59]Well, I could stand up straight, get a real job [02:43.25]Stay up late with the same old mob [02:47.16]But it hasn't crossed my mind [02:51.79]Lately [02:55.97]Put on a suit, work downtown [03:00.12]Then come up when the sun goes down [03:03.88]No, I haven't had the time [03:08.50]Lately [03:12.70]Lately I've been stayin' at home [03:20.37](Stayin' at home, stayin' at home) [03:21.06]Closin' the curtains, play jazz on trombone [03:24.95](Jazz on trombone, jazz on trombone) [03:32.55]And I dream I'm on vacation [03:36.79]No, you won't see me around [03:41.00]It's a perfect situation [03:45.37]For me [03:49.77]I don't mind being by myself [03:53.68]'Cause I know you'll come on down [03:57.59]It's the last good time in town [05:12.71]Lately I've been stayin' at home [05:16.58](Stayin' at home, stayin' at home) [05:20.72]Workin' the crosswords, turn off the phone [05:24.88](Turn off the phone, turn off the phone) [05:32.65]And I dream I'm on vacation [05:36.68]'Cause I like the way that sounds [05:40.96]It's a perfect occupation [05:45.20]For me, yes it is [05:49.85]I don't mind being by myself [05:53.75]If you don't see me around [05:57.75]It's the last good time, last good time in town

钛：最后好时光在城市 [按：1223_dd] [00：00.01]鹰-最后好时光在城 [00：20.02] 1223_dd制作 [00：58.45]我想现在出去，然后每 [01：02.30]我不能等待再次做 [01：06.19]但我没有时间 [01：10.81]最近 [01：14.27]我想退了，而在每一次 [01：18.89]我有点像做有声有色 [01：22.90]我没有时间 [01：26.96]最近 [01：31.70]最近我一直留驻'在家 [01：35.60]（留驻'在家里，留驻'在家） [01：39.73] Workin'的纵横字谜，关掉手机 [01：43.85]（关闭手机关闭，关闭手机） [01：51.71]我的梦想我在我休假 [01：55.86]'原因我很喜欢的声音 [01：59.98]这是一个完美的职业 [02：04.27]对我来说 [02：08.90]我不介意由我正 [02：12.72]如果没有其他人靠近 [02：16.69]这是最后一次在城里好 [02：38.59]嗯，我可以挺直腰杆，得到一份真正的工作 [02：43.25]保持与老暴徒晚 [02：47.16]但一直没有干扰过我 [02：51.79]最近 [02：55.97]关于提起诉讼，把工作市中心 [03：00.12]然后提出时，天黑了 [03：03.88]没有，我没有时间 [03：08.50]最近 [03：12.70]最近我一直留驻'在家 [03：20.37]（留驻'在家里，留驻'在家） [03：21.06] Closin'的窗帘，玩爵士长号 [03：24.95]（爵士乐长号，爵士的长号） [03：32.55]我的梦想我在我休假 [03：36.79]不，你不会看到我周围 [03：41.00]这是一个完美的情况 [03：45.37]对我来说 [03：49.77]我不介意由我正 [03：53.68]'的原因，我知道你会来的下降 [03：57.59]这是最后一次在城里好 [05：12.71]最近我一直留驻'在家 [05：16.58]（留驻'在家里，留驻'在家） [05：20.72] Workin'的纵横字谜，关掉手机 [05：24.88]（关闭手机关闭，关闭手机） [05：32.65]我的梦想我在我休假 [05：36.68]'原因我很喜欢的声音 [05：40.96]这是一个完美的职业 [05：45.20]对我来说，是有 [05：49.85]我不介意由我正 [05：53.75]如果你看不到我周围 [05：57.75]这是最后的好时机，最后在城里的好时机

The main factors affecting the soil-structure interface behaviors were found experimentally and theoretically, including: 1 the thickness of the interface that is five to six times the average grain size of the soil; 2 the aeolotropy of interface, which is responsible for anisotropic response of the stress-strain response of the interface; 3 two physical states, including crashing and compression of the soil near the structure surface, which govern the stress-strain response of the interface strongly; 4 two shear deformation components due to sliding and constraint of the structure surface relative to the soil respectively, which forms the deformation of the interface; 5 the volumetric strain due to dilatancy, which is found to be composed of a reversible dilatancy component and an irreversible dilatancy component. 4. A unified constitutive model of the interface, based on new elasto-plasticity damage theory, was developed. It was confirmed to be effective for the conditions considering monotonic and cyclic shearing, coupling effect of shear and volumetric strains, evolution of physical state, micro-structure aeolotropy of the soil and the resulting aeolotropy of the interface as well as the three normal boundary conditions stated above. 5. 2D and 3D finite element formulations of the present model were derived and incorporated into the FEM codes. They were applied to the evaluation of practical engineering problems with different typical interfaces between soil and structure. The new model was shown to be reasonable and effective.

确定了粗粒土与结构接触面厚度约为5～6倍的平均粒径，首次揭示了接触面的细观结构异向性以及由此所引起的宏观剪切异向性，发现了在单调和往返剪切荷载作用下土颗粒破碎和剪切压密两种物态变化机制共同支配着接触面力学性质的变化，通过细观分析证实了接触面的变形可分解为一般同时发生的土与结构交界面上的滑移变形以及结构面位移约束范围之内土体本身的剪切变形两部分，观测到接触面受剪时表现出明显的相对法向位移，并可分解为可逆性和不可逆性两个分量；(4)建立了第一个能够统一地描述单调与往返剪切特性、剪应变与体应变耦合特性、细观结构和宏观剪切异向性以及土颗粒破碎等物态变化特性的土与结构接触面弹塑性损伤本构数学模型，并采用多种法向边界条件复杂加载路径的试验成果验证了新模型的合理性和有效性；(5)提出了新模型的二、三维有限元格式并结合实际边值问题进行了应用计算分析，比较了不同接触面本构模型对计算结果的影响，证实了新模型及其有限元格式不仅能够合理地描述土与结构接触面的主要力学特性，还能够较好地反映土体与结构物在接触面处的滑移、脱开等不连续现象。

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。

With the northern slope of the Qilian Mountains high to low altitude, soil types in order for the development of alpine cold desert soil, alpine meadow soil, sub-alpine meadow soil, chernozem (slope for the dust-color), chestnut soil, ash calcium Soil.

祁连山北坡随着海拔高度由高到低，土壤类型依次发育为高山寒漠土、高山草甸土、亚高山草甸土、黑钙土、栗钙土、灰钙土。

Results showed that the topsoil structure of the CK treatment was dense with little porosity developed, and the soil microstructure was sandy granular fabric - granular fabric. In these treatments using chemical fertilizers only, the soil particles did not form soil structure with little porosity, and the soil microstructures in the N, NP or NPK treatment were observed as prophyropectic fabric-fine sand agglomerplasmic fabric, much better than the CK treatment. In those treatments receiving farm manure alone or farm manure plus chemical fertilizers, the quantity of groundmass increased obviously. The soil had a loosen structure, higher porosity, enriched animal and plant residua, iron-manganese nodules and humus, and more micro-aggregates developed. The soil microstructure of the MNPK treatment was pectized-compacted takyric fabric-intertextic fabric, the best microstructure observed among all the treatments.

结果表明：长期不施肥料的CK处理，土壤耕层结构致密，很少有孔隙发育，土壤微结构为结构较差的碎屑聚积状-沙粒聚积状；长期单施化学肥料，土壤颗粒未形成结构体，少孔隙，土壤微结构主要为斑晶胶凝状－细沙粒聚积状结构，土壤结构比CK处理优；长期施用有机肥或有机无机肥料配施的处理，土壤粗颗粒数量显著增加，结构疏松，孔隙量大，动、植物残体丰富，有铁锰结核和腐殖质的形成和微团聚体的发育，土壤微结构类型以MNPK处理最好，为胶凝紧实状－多孔状结构。

From these researches as above, this paper found a new method to analysis salty soil road engineering properties by phase equilibrium theory, which provides a new angle of analysis on salty soil properties, experiment and engineering practice in these ways as follows:(1) Analysis the disadvantage of traditional salty soil experiment;(2) Analysis the disadvantage of current salty soil definition by phase equilibrium theory, and gives the chart of distinguish salty soil by the condition of hydrography and climate change;(3) Analysis the mechanics of subgrade frost boiling based on the change rule of liquid content;(4) Based on the change rule of ingredients content and volume in salty soil, analysis the mechanics of subgrade salt heaving and the restraining method by adding sodium chloride.

通过以上研究，本文初步建立了以相平衡理论为核心的盐渍土路用工程性质分析方法，该方法对盐渍土工程性质的理论分析、试验研究以及工程实践提供了新的研究思路与方法，具体体现在：(1)分析了传统的盐渍土试验存在的缺陷；(2)分析了现行盐渍土定义的不足，并以相平衡理论为基础，结合水文、气候条件的变化给出了判别盐渍土的诺谟图；(3)分析了盐渍土盐溶液含量的变化规律，并从盐渍土含液量变化规律出发，分析了盐渍土路基较非盐渍土路基翻浆严重的机理；(4)分析了盐渍土各固相含量及其体积的相变规律，并在此基础上分析盐渍土路基的盐胀机理，以及采用添加氯化钠来抑止硫酸盐盐渍土的盐胀机理

This paper systematically summarized and analyzed general development characteristics of soil profile CaCO3 in Loess hill gully area including source, content, forming-condition, distribution and illuviation- depth of CaCO3, which will have the most important significance for the further studies on global soil and climate change.Soil CaCO3 eluviation-illuviation is a relatively complicate process, soil CO2 is one of the important effect factors, which influences soil CaCO3 through controlling soil pH value and CaCO3 solution capability.

碳酸钙在土壤剖面中淀积的深度和类型是黄土高原土壤发育的重要标志，钙积层是黄土高原土壤发育环境的历史信息库，同时土壤碳酸钙作为土壤无机碳库重要组成，它通过溶蚀后再结晶与大气CO_2之间进行物质交流来影响全球气候变化。

But this is impossible, as long as it is engaging in a market economy, there are risks in any operation.

但是，这是不可能的，只要是搞市场经济，是有风险的任何行动。

We're on the same wavelength.

我们是同道中人。