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风化层

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On the basis of making it clear that laterization includes such three integrated stages as weathering, micro-granularity and soil formation of laterite, the thesis illuminates characteristics of Kunming laterite in chemical composition, physical mechanics, composition of granules, fractal dimension of granularity and the connection of granules. The experiment using soil reinforced agent to solidify the laterite shows that the mechanical traits of laterite have been improved because of its involvement, the best compact indicators and shear strength ones increased and the indicators of laterites penetrability and compression decreased. The effects of reinforcement can be weighed through its coefficient and the mechanism of reinforcement can find the explanation in the effect of soil reinforced agent on the laterite granules, the changes in the electric double layer caused by soil reinforced agent and its enwrapping of laterite granules.

在明确红土化作用包括风化作用、微团粒化作用以及红土成土作用三个完整阶段的基础上,阐明了昆明红土的化学组成特征、物理力学特征、颗粒组成特征、颗粒粒度分维特征以及颗粒连接特征;土壤强固剂加固红土试验表明,土壤强固剂的加入,改善了红土的力学特性,提高了红土的最佳击实指标和抗剪强度指标,减小了红土的渗透性指标和压缩性指标,其加固效果用加固效果系数来衡量,其加固机理可用土壤强固剂与红土颗粒之间的物理化学作用、土壤强固剂引起红土双电层的变化以及土壤强固剂对红土颗粒的包裹作用来解释。

Carbon dioxide layers have been encountered in the Ordovician weathering crust of Lower Paleozoic and in Es13 of Paleogene.

东濮凹陷在下古生界奥陶系风化壳与下第三系Es13地层发现了高含CO2气层。

The natural releasing processes of Pb, Zn and Cd in the slags can be primely described with minus-exponent equation.

长期的风化淋滤作用对重金属的释放有影响,矿渣层的重金属含量随时间的增长而递减,其自然释放过程可用负指数方程描述。

The smooth sculpture-like exterior of the Pavilion is an image of the arc-shaped rocks rolling endless in Australia's countryside; its exterior wall uses special weather-resistant steel cladding materials the color of the curtain wall will deepen over time until it turns the color of reddle much like the red earth in Australian inland.

澳大利亚馆流畅的雕塑式外形好似澳洲旷野上绵延起伏的弧形岩石,外墙采用特殊的耐风化钢覆层材料,幕墙的颜色将随时间的推移日渐加深,最终形成浓重的红赭石色,宛如澳大利亚内陆的红土。

The color difference between saprolite blocks and their parent rocks is obvious and the texture and structure of the parent rock can be preserved in saprolites.

发育于斜坡非饱和带的结晶岩与碎屑岩腐岩多夹于残坡积土层和风化岩带之间,保留有裂隙及层理等构造,但质地松软。

Analyze the failure models of rock slope, and then classify the sliding plane, the sliding plane can be divided into self-born sliding plane, appendiculate sliding plane and mixed sliding plane, furtherly summarize the selection method of mechanics parameters to each types. Based on the classification, the author establishes the mechanics model of each sliding plane. Discuss the influence of water and weathering and sedimentation conditions on rock slope, and then specify the geological cause of rock bedding slope, counter-tilt rock slope and cracked rock slope.

2分析了岩质边坡的几种主要破坏模式,在此基础上对岩质边坡滑动带进行分类研究,从大的方面主要分为自生型滑动面、依附型滑动面和混合型滑动面三类,总结与各类滑动面相适应的力学参数取值方法,从而建立岩质边坡滑动面的力学分析模型,讨论水、风化和沉积环境对岩质边坡的影响,归纳了顺层岩质边坡、反倾岩质边坡和破碎岩质边坡滑动面的成因。

The source of slack deposits is the loess of the upper reach where the soil erosion is very heavy, while the source of sand is the airslaked rocks of mountainous area in the upper reach. 3. There were several "interbedded slack deposit-aeolian fine sand layers" in both LHT and YWC profiles, the silt layers are slack water deposits and the aeolian fine sand layers were carried by the NE direct wind.

在LHT、YWC和YYC剖面中,磁化率均呈现出平流沉积层中偏低,而在风吹沙和中、粗沙层中偏高的特点,其原因是平流沉积层的物质来源多为上游黄土区的土壤侵蚀和水土流失带来的土壤,而沙层的物源则是上游基岩山区的岩石经风化、搬运而来。

Photo Gallery: Erosion and Weathering Wind erosion makes these layered sandstone hills swirl in Paria Canyon-Vermilion Cliffs Wilderness Area.

意译:侵蚀和风化的图片画廊。风蚀使这些层状的砂岩丘陵漩涡中帕里亚峡谷,朱红色悬崖荒野地区。

Different models for different structure sections are established, namely, one-dimensional piping model for laneway or large hole, two-dimensional structure plane model for absciss layer and contacting weathering zone, three-dimensional seeping fracture section model.

分区建立了采空区不同注浆结构部位的理论模型,包括采空区空洞或巷道的一维&管道&模型、离层与接触风化带等结构面二维模型、导水裂隙带三维模型。

Evidence of emergence including sabkha dolostone, algal mat, bird-eyes and fenestral structure, mudcracks and crustose limonite has been found in the top of the Changhsingian reefs in Ziyun, Guizhou province.

贵州紫云长兴期生物礁顶部存在的出露证据有:(1)形成于萨勃哈蒸发环境的白云岩,(2)藻纹层沉积,(3)鸟眼和窗格构造,(4)干裂缝和褐铁矿风化壳,等等。

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