巖川 的英文怎麼說

中文拼音 [yánchuān]
巖川 英文
iwagawa
  • : 名詞1. (巖石) rock 2. (巖峰) cliff; crag
  • : 名詞1 (河流) river; stream 2 (平地; 平野) plain: 800里平川 a vast eight hundred li plain; 米...
  1. They are jinfo mountain in nanchuan county ( natural protection section ), wuling mountain in qianjiang county ( national emphases forest demonstration county which forest cover rate is beyond 50 % ) and zhongliang mountain in beibei county ( artificial destruction is very grave ). some main land use patterns i. e. woodland, garden, infield, abandon infield, shrub and grassplot are selected in those three sample sites. four aspects on soil fertility index of karst environment under different land use patterns in these three sample sites, are revealed in this paper, by using the field test, indoor measure and analysis, outdoor experiment and field investigation, and the knowledge and technique of soil, ecology, physics and chemistry etc. they are physical characteristic ( effective soil thickness, organic layer thickness, soil texture, water - stable aggregate and soil water etc. ), chemical fertility ( organism, omni - n, omni - p, omni - k, alkali - nitrogen, available p, available k and rapid available k etc. ), soil animalcule ( bacteria, fungi, actinomyces and their grosses ) and soil - seed - pool ( plant community diversity index ) in karst ecosystem

    本研究以重慶市的南金佛山(自然保護區) 、黔江武陵山(國家重點退耕還林示範縣,森林覆蓋率50以上)和北碚中梁山(遭人為破壞嚴重)典型溶區為對象,選擇了幾種重要的利用方式,包括林地、果園、耕地、棄耕地和灌草坡,採用野外溶生態調查和室內試驗測量分析相結合的方法,以不同土地利用方式溶土壤肥力為重點,對不同土地利用方式土壤肥力特徵進行量化分析,找出溶土壤肥力差異的主要方面及其根本原因,論文主要從土壤剖面物理退化指標(有效土層厚度、有機質層厚度、質地、團聚體、水分含量等) ,化學肥力退化指標(有機質、全n 、全p 、全k 、堿解n 、速效p和速效k等) ,樣地土壤微生物指標(細菌、真菌、放線菌數量及總量)以及樣地土壤種子庫植物群落多樣性等4個方面對重慶典型溶區的土壤肥力特徵進行了較為詳細的分析研究,為溶地區士壤資源的合理利用及結構的調控管理提供依據。
  2. Relationship between anisotropy of jinchuan rockmass and deformation and failure of adit

    體各向異性與巷道支護變形破壞關系探討
  3. Rocks of assorted sizes and shapes are embedded in the bottom of a glacier.

    多種尺寸和形狀的石都埋藏在冰的底部。
  4. In view of bearing capacity of the elastoplastic theory analysis, the author made a comparison between the achieved bearing capacity limit load pi / 4 of round base ( space problem ) and the limit load pi / 4 of bar groundwork foundation design ( plane problem ) from soil mechanics at home and abroad as well as foundation criterion, and explained why the value of formula in present design criterion from soil mechanics is inclined to be conservative. in the light of the author ' s many years experience of vibration test on the spot and the research work of relevant projects, the author worked over the dynamic pile testing of the bearing capacity of foundation and batholith, and gathered the parameter of dynamic analysis and testing. the author also talked over the difficult point of pile foundation design criteria in present batholith engineering world, i. e. the confirmation of batholith bearing capacity of pile end, from the following aspects : a ) confirmation of single axis counter - pressure strength of rock in house ; b ) f. e. m calculation of elastoplastic model ; c ) calculation of soil mechanics ; d ) deep well load test

    然後,對土工程領域至今尚未解決,甚至不為人注意的考慮地基變形的地基承載力問題進行了實用化的探討,提出了考慮地基變形的地基承載力上程計算方法;對基於彈塑性理論分析的地基承載力國內尚未見報道的空間問題得到了圓形基礎(空間問題)的承載力界限荷載p _ ( 1 / 4 ) ,並與國內外土力學專著及地基基礎設計規范中的條形基礎(平面問題)的界限荷載p _ ( 1 / 4 ) ,進行了對比,從而定量上解釋了目前設計規范引用土力學承載力公式值偏於保守的這一情況;根據本文作者多年從事現場地基工程振動試驗及相關課題的研究工作,本文以截頭錐模型模擬地基,對地基(基)承載力的動測法進行了研究,為各類地基(包括基) ,匯總了動力分析和檢測的參數:針對日前土工程界應用樁基設計規范中的難點? ?樁端基承載力的確定問題,從石室內單軸抗壓強度確定、基於彈塑性模型的有限單元法計算、土力學計算及深斤載荷試驗四方面進行了深入討論;本文作者根據多年現場載荷試驗的工程實踐,對深井荷試驗裝置的核心部分? ?反力裝置,設計了側壁支撐反力加載系統,該加載系統具有實用、簡便、穩定及安個等優點。
  5. Under the guidance of the theories of sedimentation, paleontology, stratigraphy, reservoir geology and digenesis, synthetically applying the methods of the conjunction of spot - line - surface, macro - microscopic and field - indoor, there is a comprehensive study for the upper permian series in stratum, rock, sedimentary facies and diagenesis, especial for the type and characteristics of sedimentary facies, in the paper. based on the above, the vertical evolutionary model of the sedimentary environment is explained by the study of the elevation profile and transverse profile and the regional geological characteristics

    本文主要是以沉積學、古生物學、地層學、儲層地質學等相關理論為指導,運用點線面、野外與室內、宏觀與微觀相結合的方法,並藉助普通顯微鏡、陰極發光顯微鏡等手段對西地區北部上二疊統的地層、石、沉積相以及成作用進行了研究,尤其是對沉積相的類型及特徵作了詳細的劃分與闡述。
  6. The geologic, element and experimental study suggest the mechanism of small body, giant deposit in jinchuan is succeeding segregation whole magma chamber intruding from deep to emplace. the study is proof, supplementary and progress of the deep segregation, penetrating ore formation theory, which was advanced by mr tang zhongli, the academician of china. 5

    特別是通過鉑族元素、稀土元素研究、實驗地球化學研究及其與實際資料的對比,提出了金礦床成成礦是從深部到侵位持續熔離的新模式,論證、補充和發展了湯中立院士提出的深部熔離成礦說。
  7. Rock underlying glaciers is eroded by plucking.

    下面的石則是通過拔削作用被侵蝕的。
  8. The yanchang formation of upper triassic in north shaanxi is major terrigenous clastic system deposited in fluvial - latchstring environment, under the influence of the llocyclicity factor which include indosinian tectonic, eustacy, sedimentary supplies and the autocyclicity factor. in late triassic, north shaanxi was divided into two parts bounded by zhidan - ganquan - yichuan demarcation line

    陜北地區上三疊統延長組是以河流一湖泊相為特徵的陸源碎屑系,當時的陜北地區,以志丹?甘泉?宜沿線為界,南側以明顯的斜坡向深湖盆地過渡,北部則為一地形平緩的淺水臺地。
  9. Based on 3 - d seismic well and logging data, mainly by means of advanced seismic theories of reservoirs prediction and other corelational multidisciplinary, an extensive and indepth studying on the tight sandstone reservoir with fracture of the second part of the xujiahe formation in west sichuan depression has been carried out. a series of theoretical viewpoints and research fruition are concluded as follows :. 1 on the basis of analysis of the regional and local structure characteristics and evolution, a conclusion comes in to being : inchoate and nowadays structure traps and the match model between structure and fracturation system are the main factors in controlling the formation of effective traps

    本文綜合利用三維地震、鉆井、心、測井資料,採用地震儲層預測方法為主線的多學科綜合研究思路對西坳陷上三疊統須家河組二段緻密裂縫性砂儲層進行了較為廣泛、深入的研究和探索,取得以下一系列理論認識和研究成果: 1 、通過區域及局部構造特徵及構造演化史分析,認為古今構造圈閉、構造與斷裂系統配置關系是控制有效圈閉形成的主要因素。
  10. Fission track geochronology of xiaonanchuan pluton and the morphotectonic evolution of eastern kunlun since late miocene

    東昆侖山小南體裂變徑跡年代與中新世晚期以來的構造地貌演化
  11. These ridges formed by glaciers or lava flows are called moraines.

    由冰和熔形成的側脊叫冰磧。
  12. Comprehensive study indicates the dark, 50 - 300 m thick upper permian series, which is rich in the organic material ( om ) and biota, is beneficial to formation and protection of petroleum and natural gas. moreover the stratigraphy possess with better reservoir ability. the reservoir distributed in shallow glacis along beichuan tongkou - guangyuan changjianggou, he 12 well - she 1 well - jiange - cangxi yongningpu - long 4 well - bian 1 well in wujiaping stage and in platform edge beach along beichuan tongkou - jiangyou shuigentou - jiange - cangxi yongningpu - nanjiang

    綜合以上,本文認為研究區上二疊統地層厚50 ? 300m ,顏色較深、生物含量多、富含有機質,並且該套地層自形成后,大多直接進入埋藏成環境,是一套十分有利於油氣的形成與保存的地層;同時該套地層的局部層段具有一定的儲集性能,在吳家坪期儲層主要分佈在北通口?廣元長江溝、河12井?射1井?劍閣?蒼溪永寧鋪?龍4井?扁1井一帶,在長興期儲層主要分佈在北通口?江油水根頭?劍閣?蒼溪永寧鋪?南江一線。
  13. Lithogeochemistry and lithogenetic epoch for shaba granulite in mianning, sichuan

    冕寧沙壩麻粒石地球化學性質及形成時代
  14. Igawa is the third japanese player posted this winter, joining matsuzaka and infielder akinori iwamura, whose rights were acquired by the devil rays for about $ 4. 5 million

    慶是今年冬天第三位開放競標的日本選手,前兩位分別是松坂大輔和內野手村名憲,這名內野手稍早由魔鬼魚隊以450萬美金得標。
  15. The research of large igneous rock province - ermei basalt extrusion - mantle plume shows that songpan - ganzi folded belt is a hopeful target for breakthrough of petroleum exploration, and the key issue is how to make well a coupling and optimization among its faults, structures, traps and reservoirs

    根據地震測深、重、磁、電等的探查,發現該褶皺帶深部有一低速高導層,而對大火成省峨眉玄武噴溢地幔柱的認識深化均表明,四松潘甘孜褶皺帶是可望獲得油氣勘探突破的靶區,重要的是斷裂構造、圈閉、儲集層的耦合與優化。
  16. It ' s a kind of dead soft - rock with some special characteristics of muddiness, softenness, dehydrate and rift etc when it meet water. however, the articles about the socketed piles in this stratum had not been discovered

    昔格達組泥在四境內的西昌、攀枝花地區分佈較為廣泛,該層具有遇水泥化、軟化和脫水開裂等特徵,屬極軟類。
  17. The paper adopts some methods such as gas composition, carbon isotope, systematical analyzing and testing of reservoir bitumen biomarker from high evolutional natural gas and quantitative calculation of mixed gas, illustrates that natural gas from the section of jialingjiang formation is mainly attributed to sapropel type organic matter gas of permian, comes from carbonatite hydrocarbon rocks permian which most of them are overmature, its main gas source has nothing to do with carbonatite hydrocarbon rocks of jialingjiang formation themselves, presents in geochemistry characteristics of oil type cracked gas

    摘要通過對南過渡帶西部的磨溪潼南地區嘉二段天然氣組成、碳同位素組成、高演化天然氣儲層瀝青生物標志化合物的系統分析測試和混合成因氣的定量估算,闡明了該區嘉二段天然氣主要屬於二疊系腐泥型有機質成因氣,來源於二疊系過成熟為主的碳酸鹽烴源,主力氣源與嘉陵江組自身的碳酸鹽烴源無關,並具有油型裂解氣的地球化學特徵。
  18. Testing study of subcritical crack growth of ore in jinchuan mine

    亞臨界裂紋擴展試驗研究
  19. The sankeng geothermal field is located on the northeastern side of the wuchuan - sihui deep fault and in the sankeng synclinal karstic basin

    摘要廣東三坑地熱田位於吳四會深大斷裂帶的東北側,三坑向斜溶盆地內。
  20. Then cross the dutch border to the rhineland, germany. at the picturesque rhine valley, roam past medieval castles, half - timbered houses and vineyards to loreley rock, where we will have a german feast by the river rhine

    驅車經全德國最大工業區魯爾,再前往世界最重要的河-萊茵河,兩岸古堡星羅棋布,葡萄園山坡引人入勝,羅樂萊石更添神秘色彩。
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