salt formation 中文意思是什麼
salt formation
解釋
鹽層建造-
Distribution, formation and characteristics of the saline - alkalized land in northeast china was systematically analyzed and agro - biological measures for management of saline - alkalized soil were illustrated, including cultivation of rice to wash down salts, cultivation practices, soil building practices, plantation of salt - tolerant plants and biological removal of alkali, etc. in the paper
特殊的氣候、地形和水文地質等自然因素以及人類不合理的農業技術措施和社會生產活動等人為因素加劇了該區鹽堿化發生、分佈與演變。 -
On the formation of the moral dedication and remuneration system, encouraging the salt of the earth. punishing the devilry man, which is good for advancing civil moral diathesis. administing the party by moral is a key to ruling country by virtue. party pioneer exemplar has important effect on socialist mores
建立道德奉獻與回報機制，對道德高尚的人進行獎勵，保障他們的道德權力，同時對那些惡行進行懲罰，這是提高培養公民的道德素質的有效途徑。以德治政，是以德治國的關鍵，黨員的先鋒模範作用，對社會風氣的好轉起著至關重要的作用。 -
The investigation of a lot of parameters about treated sandstone, brick materials and earthen materials with fluorited polymers has been carried out, such as the formation of polymer, the penetration depth, porosity, capillary absorption and penetration coefficient, water uptake, compressive strength, drilling resistance, absorption isotherms of water vapor, water vapor diffusion, color changes as well as resistance to desegregation of water, frizzing - throwing cycles, worming - cooling cycles, and so on. in addition, the influence of salt crystallization, acid and base, and uv aging have also been assessed in order to better understand the protection effects and utilization possibility of two fluorinated polymers, mainly according to astm standard and the combination of international methods together with general technological
分別以國家級文物保護單位的土質、砂巖和磚材文物樣品為對象，依據astm標準及國際通用文物保護研究方法與評估準則相結合，通過膠化物形成周期、滲透深度、孔隙度、毛細吸水和滲透系數、持水量、抗壓強度、抗鉆強度、吸附水蒸氣的能力、透氣性、外觀顏色等系列參數的測定，及凍融、冷熱循環、酸堿腐蝕后抗壓強度的衰減、可溶鹽對保護效果的影響、酸堿及光照對表面保護效果的影響，對兩種含氟聚合物及其與有機硅的共混物在文物加固保護和表面防護中的可行性和保護效果給予了系統研究。 -
In middle and late periods of the early permian, the pre - caspian areas rose successively, the climate became dry, and the environment turned to be supratidal zone ( evaporitic environment ), resulting in the spread sedimentation of salts and the formation of the salt sediment group ( the upper part of the lower permian ) which consists mainly of halite and anhydrite
早二疊世中後期由於持續構造抬升，盆地氣候變得乾旱，海水變淺，潮上帶蒸發環境發育，以致這一時期廣泛發育鹽類沉積，形成含鹽層系，主要由鹽巖和硬石膏層構成，並形成許多大小不等的鹽丘構造。 -
Besides, the sedimentary facies of upper ganchaigou and lower ganchaigou formation were also mapped in supersequences which are the main target strata for exploration. the high resolution sequence stratigraphic framework showed the genetic relationship between the distributions of sedimentary facies and their tectonic settings. the near - source sedimentary systems such as subaqueous alluvial fan and lake - floor fan are often deposed in rise - hemicycles in the steep slope background in the north, the coarse lithology of fan - delta prograded from north to south in fall - hemicycles, and the braided stream facies are formed in the rise - hemicycles in gentle slope background in the south, braided stream facies prograded from sorth to north in the fall - hemicycles, but the lacustrine facies and salt lake facies developed in the middle part of the area
詳細的沉積相研究發現，紅獅地區第三系發育有沖積扇、水下沖積扇、河流、三角洲、扇三角洲、湖泊和湖底扇7種主要沉積相類型，並對作為區內主要勘探目的層系的下乾柴溝組和上乾柴溝組進行了以超層序為單位的沉積相平面編圖，以較高的時間解析度揭示了區內沉積相帶的平面展布及其在不同構造背景中的分佈規律，比如在北部的凹陷陡坡背景下，上升半旋迴低水位期通常發育有水下扇、湖底扇等陡岸近源特徵的沉積體系，下降半旋迴高水位期，扇三角洲相粗碎屑巖由北向南進積;在南部的凹陷緩坡背景下，上升半旋迴主要發育辮狀河流相，下降半旋迴辮狀河三角洲相由南向北進積;而中部紅柳泉一獅子溝一帶則為湖泊相沉積和鹽類沉積。 -
Application of flac in borehole shrinkage in formation of plaster stone and salt stone
鹽膏巖地層的井眼縮徑變形分析 -
Large - scale exploration of the salt mine resources and numbers of migration were the two primary influences on its formation
在這些市鎮的形成過程中，大規模礦產資源的開發和大批前來從事采礦的外省移民的湧入是其成因的兩大主導因素。 -
The formation of salt - alkaline soil included salinization and alkalinization. the increase of salinity was the character of salinization, and the increase of ph was the character of alkalinization
土壤的鹽堿化即包括土壤的鹽化又包括土壤的堿化，鹽化以上壤鹽度升高為特徵，堿化以土壤ph升高為特徵。 -
It will be both practical value and theoretical significance to systematically research the causes of formation, sources of salt, and development regulations of the thick beds of salt rocks in puwei sag, and to probe into the relationship about salt and oil and gas accumulations, under the direction of sequence stratigraphy and sedimentology theorys and metheds, conbined with the analyses of the colligation of structures and strata, geophysics, geochemistry, basin analysis, and oil and gas bearing systems theorys and methods, on the basis of the synthesis analyses and dissections of cores, logs and seismic data
以層序地層學與沉積學的基本理論和方法為指導，綜合構造?地層分析、地球物理學、地球化學、盆地分析、含油氣系統的理論和方法，通過鉆、測井資料和地震資料的綜合分析和詳細解剖，對該窪陷鹽巖的成因、鹽源及其發育規律進行系統研究，並分析探討該地區鹽巖與油氣聚集的關系，不僅具有實踐價值，而且具有理論意義。 -
This paper studied the effect of soil water content on barley at different growth stages, through the study, we found the sensitive stages of barley to water and salt is the stem elongation and spike formation stages
研究表明，大麥對水鹽最敏感時期發生在拔節抽穗期，土壤含水量（占飽和含水量的體積百分數）上限值確定為80 . 4 ，耐鹽漬天數為3 . 2天。 -
This is the other main reason for the overpressure in kuche depression to be preserved. we analyzed the effect of fracture in the gas deposit formation and hold that different kinds of fracture have different effect : hydrocarbon dissipation and relief effect of crossing salt bed faults that run through source rock, reservoir, and caprock ; filling effect of under salt bed faults that run through source rock and reservoir ; slippage faults that did not connect source rock have no effect to hydrocarbon accumulation and dissipation ; adjusting faults in reservoir have effect of adjusting formations for hydrocarbon distribution
分析了斷裂在天然氣成藏中的作用，認為不同類型的斷裂在天然氣成藏過程中的作用是不同的：貫通生、儲、蓋層的穿鹽斷層對油氣散失和泄壓作用；貫通源巖和儲層的鹽下斷層對抽氣運聚的充注作用；不連接源巖的滑脫斷層對油氣聚散無作用；儲層內調整斷層對油氣分佈起調整層位作用。 -
The alternative changes of paleoenvironment favored the formation and imbedding of brine, which is the source of salt - water intrusion ; and the paleochannel that formed during regressive of sea level is the path of salt - water intrusion
海進時期，大面積的濱海平原被淹沒，在近海平原窪地滯留的海水經過蒸發、濃縮變為鹵水，成為鹹水入侵的物源；海退後陸源碎屑在濱海地區沉積形成了巨厚的古河道砂層。 -
Origin of 3rd member salt rock of shahejie formation in dongpu sag
東濮凹陷沙三段鹽巖成因 -
2 the salt - resistant characteristic which is adapt to depressed level of photosynthesis, such as the formation of double palisade tissue, and soon
適應光合水平降低的抗鹽結構特徵。如莖皮層同化組織的形成；葉片雙側柵欄組織或外周柵欄組織的形成等。 -
The wetland is being provided as an ecological mitigation measure for the land formation of the reserve zone and will form a buffer between the new town and the ramsar site at mai po marshes. the hong kong wetland park project is the first of its kind in hong kong and will provide a range of fresh and salt - water habitats for establishing wildlife
這幅在香港首次建造的濕地，可緩解預留區土地開拓工程對生態的影響，並為天水圍新市鎮與米埔沼澤區拉姆薩爾濕地提供緩沖區，而濕地的咸、淡水環境更可供野生生物繁衍棲息。 -
It is considered that the sedimentary structures of pukou formation in huaiyin nag are different from those in yanfu depression, and the new characteristics of salt rocks of over 1000 m thickness appear in this area
認為淮陰凹陷浦口組和鹽阜坳陷有不同的沉積構造特徵，特別是本區發育的厚度達千米的鹽巖沉積，更有其特殊性。 -
Beginning with the analyse of present situation and cause of formation of saline - alkali land, the irrigated area overall water salt trends are analysed, and the irrigated area saline - alkali land and the groundwater level and distribution law of groundwater degree of mineralization are expounded, the trendence of irrigated area saline - alkali land is put forward. then water salt balance model is estanbished according to the relationship of irrigating and drainage. regarding the irrigated area as a balance area, by analysis of mineralization degree of water pumping from the yellow river and drained off water from irrigated area, the change of the draining off water ion is forcasted in water reducing condition
課題研究主要從鹽堿地現狀與成因及灌區總體水鹽動態分析兩方面入手，闡述了灌區鹽堿地、地下水位、地下水礦化度的分佈規律，分析了灌區鹽堿地的成因及變化趨勢；根據灌區灌溉、排水條件與以上各種因素的關系，建立了灌區水鹽均衡模型；把灌區作為一個均衡區，通過對黃河來水礦化度、灌區排水礦化度的分析，預測了在灌溉引水、排水減少時排水離子量的變化；運用灌區水鹽動態模型原理，對灌區現狀（ 1998 、 2000年）與規劃水平年總體水鹽平衡進行了計算；總結分析了灌區水鹽動態變化趨勢，計算並提出了排水控制標準。 -
In this paper irrigated area water salt balance and the trends change is studied, the cause of formation and the trendence of saline - alkali land is analysized ; the foundmental theory for the administration of saline - alkali land is provided
本課題通過研究灌區水鹽平衡和動態變化，分析灌區鹽堿地的成因及變化趨勢，為鹽堿地治理提供一定的理論基礎，對解決灌區實際問題具有指導意義。 -
The formation mechanism of mash scale is the following : slightly soluble or soluble substances in hypersaturated state separate out during distillation, soluble calcium salt converts into calcium carbonate scale or soluble calcium salt resolves into indissoluble calcium carbonate scale by heating
摘要醪垢的形成因素有：微溶或可溶物質在蒸餾過程中處于過飽和狀態而析出；可溶性鈣鹽轉化成碳酸鈣垢；可溶性鈣鹽受熱分解生成難溶碳酸鈣垢；前處理的制槳工藝。 -
With regard to the causes of formation and sources of salt, people have different point of views in different basins, and different depositional models are set up, even in one same basin there are also divergent view to exist different opinions still exist on the position of the salt bearing strata in sequence stratigraphy. it will greatly influence the exploration level of resources in salt - bearing basin if the above doublts can not be made clear. in this way, it will be of great significance to make it clear about the above issues and the relationships about salt and oil & gas
對于鹽巖的成因及鹽源在不同盆地有不同的認識，並建立了各自的沉積模式，就是同一含鹽沉積盆地或含鹽沉積凹陷人們的認識依然分歧很大，關于鹽巖在層序地層中的位置人們的認識依然不同，對這些問題的認識不清將極大的影響對人們含鹽盆地的能源勘探開發水平，因此搞清鹽巖的成因及其與油氣聚集的關系具有重要意義。
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