physical weathering 中文意思是什麼

physical weathering 解釋
機械風化
  • physical : adj 1 物質的，有形的，形而下的 （opp psychical spiritual mental moral）; 確鑿的；外界的。2 身體的...
  • weathering : 大氣暴露
  1. Rubber - or plastics - coated fabrics - accelerated ageing tests - physical ageing : effect of light or weathering

    橡膠或塑料塗層織物.加速老化試驗.物理性老化:光和氣候的影響
  2. Rubber - or plastics - coated fabrics - accelerated ageing tests - part 2 : physical ageing : effect of light or weathering

    橡膠和塑料塗層織物.加速老化試驗.第2部分:物理老化.光或氣候老化作用
  3. Rubber - or plastic - coated fabrics - accelerated ageing tests - part 2 : physical ageing : effect of light or weathering ; german version en 12280 - 2 : 2001

    橡膠和塑料塗層織物.加速老化試驗.第2部分:光和風化
  4. The main factors influenced fractures development are the tectogenesis, the physical weathering and the chemical dissolution

    影響裂縫發育的主要因素是構造、物理風化和化學淋溶作用。
  5. The mainly reservoirs in the middle of damintun depression of liaohe basin are the regional metamorphic rocks and the migmatites, which are more fractured and rigid by the cataclastics. the space of metamorphite is the mainly fractures, which are produced by the tectogenesis and the physical weathering

    2 、遼河大民屯中部地區主要儲集巖是太古界的區域變質巖和混合巖類，尤以裂縫發育和經過碎裂化的剛性變質巖類的儲集性能最佳。
  6. Abstract : compared with soil destroyed pattern of vertical force and its controlled factor of bearing capacity, it is concluded that pile capacity and its tip resistence have some difference when soil with the same physical mecanic property is used as natural foundation and pile tip resistent layer. whereas the middle weathering rod stratum hasn ' t this property, that is to say it has the same bearing capacity and pile tip resistence

    文摘:通過豎向荷載下土（巖）體的破壞模式及其承載能力控制因素的比較，論述了物理力學性能相同的土層作為淺基礎的天然地基與樁端持力層時，承載力值與樁端阻力值應存在一定的差異；而中（微）風化程度的同一巖層作為天然地基與樁端持力層時，不具有這方面的差異性，承載力值與樁端阻力值應該相等。
  7. The main conclusions and cognitions are as follows : ( l ) rockmass weathering should be studied from either microcosmic and macrocosmic, microcosmic contain includes of mineralogy and of lithology, and in macrocosmic, weathering action damages integrality of rockmass, so studying rockmass structure can open out weathered degree of epigenetic - surface rockmass. ( 2 ] the dissertation sums up the characteristic indexes which can token weathered and unloaded degree, simultaneously, puts forth and summerizes several methods that classifies different weathered and relaxed zones of slope rockmass. ( 3 ) river valley epigenetic - surface reformation is controlled by rockmass structure, but weathering and unloading of rockmass is the direct cause which leads to different epigenetic - surface physical geology phenomena, for example, collapse, landslide, incline, dynam - relaxed and so on

    本文主要結論與認識為： （ 1 ）對于巖體風化的研究從微觀與宏觀兩方面入手，微觀方面重視對礦物學、巖石學的研究，宏觀方面，上升到巖體結構被改造的高度進行研究； （ 2 ）歸納了表徵巖體風化、卸荷程度的特徵指標並提出了劃分巖體風化、卸荷程度的幾種方法； （ 3 ）巖體結構控制著河谷淺表改造，但導致崩塌、滑坡、傾倒、松動等表生物理地質現象的直接原因乃是巖體的風化、卸荷。
  8. ( s ) weathering and unloading action which are the two main exogenous process is active in epigenetic - surface. so, although one is different with the other, they are associated with each other closely and are cntrolled by geostress and seepage fields. in fact, weak weathered zone corresponds to weak load - off one, strong weathered zone corresponds to strong load - off one in virtue of result of this dissertation. ( 6 ) rock mass is a geologic body which is composed of rock and structural plane. and under the condition of geostress. temperature and seepage fields, correspondingly. studying weathering should pay attation to the aspects of rock, structural plane and fields. according to this. the author subdivises rockmass weathering into rock weathering and structural weathering, ulteriorly, the dissertation studies rockmass weathering from three aspects as follows : ? ock weathering : aberrance degree of mineral and physical mechanical performance of weathered rock ; ? e have already knew that weathering action damage the integrity of rock mass, but few applies it to engineering practice. the dissertation is based on trend o

    本文研究結果為弱卸荷與弱風化大致對應、強卸荷與強風化大致對應； （ 6 ）巖體是由組成它的巖石與缺陷賦存於一定環境場中的地質體，據此本文將巖體風化細劃為巖石風化與結構面風化，並進而將表徵巖體風化的指標相應地歸結為三個方面來加以研究並應用於工程實踐，這就是：對于巖石風化，主要為礦物的變異程度與風化巖石的物理力學性能研究：雖已認識到風化作用破壞了巖體完整性，但將該理論應用於巖體風化分帶卻不多見，本文即從淺表部位硬性結構面間距、條數、跡長、塊度等隨遠離臨空面的變化規律來研究巖體風化分帶：不同風化、卸荷程度的巖體實際處于不同環境場中，彈性波速變化與特定環境場相對應，因而是反映巖體風化、卸荷的綜合因素。
  9. Through 101 landform photos, this book elaborates on the influences of bedrock, the power of water and the processes of weathering, erosion and deposition on the landforms of hong kong. this book provides a good introduction to hk s physical geography

    本書透過一百零一幅相片，闡述各種母巖水的力量及風化侵蝕沉積等作用對塑造香港地貌的影響力，是認識香港自然地理的入門書籍。
  10. The second stage is stage of the matter transfers the activated matter, that is to say, minerals build up their surface area after passing though physical weathering, maifan stone form a lot of clay mineral, oxide, oxhydroxide and collide mineral after passing though chemical weathering. it makes nutrition elements transform from crystal state to adsorption state and it expands the activation of mineral, in the latter stage, it makes maifan stone have many special physicochemical adjusting character, for example, ph and foi bi - directional absorptive and ion exchange character, so these characters expand maifan stone ' s uses

    第二階段為物質轉變的活性階段，即通過物理風化增大表面積、通過化學風化形成大量粘土礦物、氧化物和氫氧化物及膠體礦物，使營養元素由結晶態轉變為吸附態，從而大大增加了其活性。在後一過程中麥飯石還形成了許多特殊的物理化學性質，如ph值和f _ （ o2 ）的雙向調節性，吸附性和離子交換性等，從而擴大了其用途。
  11. 2 ) according to the fractures effected by tectonics, solution, weathering, rock mineral and inner rock structures, etc., understanding is given of fractural networks developed on the top of weathered crust in buried hill, and presented physical model for this networks, indicating that it is comprehensive actions by all kinds of factors that intensify fractal characteristics of the networks

    根據裂縫受構造、溶蝕、風化、巖石礦物和巖石內部結構等多因素的影響，提出了古潛山風化殼頂發育裂縫網路的認識，並給出裂縫網路物理模型，指出各種因素的復合作用，加劇了裂縫網路的分形特徵； 3
  12. The zone is formed by strong weathering of hard and rigid granodiorites formed 2. 7billion years ago, which the physical characters and chemical componentsat the surface of granodiorites have been changing posed by the geological forces of air, temperature and biology etc

    27億年左右形成的堅硬花崗閃長巖，在大氣、溫度、水和生物等外力地質作用下，其表層發生了物理性質或化學成分的變化，即強風化作用。
  13. The zone is formed by strong weathering of hard and rigid granodiorites formed 2. 7billion years ago, which the physical characters and chemical components at the surface of granodiorites have been changing posed by the geological forces of air, temperature and biology etc

    27億年左右形成的堅硬花崗閃長巖，在大氣、溫度、水和生物等外力地質作用下，其表層發生了物理性質或化學成分的變化，即強風化作用。
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