aeration zone 中文意思是什麼
aeration zone
解釋
包氣帶-
The zone between the water table and the surface is called the zone of aeration.
潛水面與地表之間的地帶稱為飽氣帶。 -
Such a traditional division of the zone of aeration is useful for illustrative purposes.
為了說明的目的，包氣帶的傳統劃分是有用的。 -
The zone of aeration may be treated more efficiently as a single moisture continuum.
包氣帶可以更有效地作為一個單一的水分連續介質來看待。 -
Under the guidance of theories of sedimentology, petroleum geology and sequence stratigraphy, and through the comprehensive analysis of outcropsrock, cores, well logs and testing outcomes of rock gas, this paper studies the depositional systems of neopaleozoic and the character of aeration zone in tabamiao area of ordos basin. the result indicates that the object layers are divided into two depositional systems, the barrier seacoast depositional systems are recognized on upper carboniferous taiyuan phase with tidal flat, lagoon and barrier bar sedimentary deposit
本文根據沉積學、石油地質學和層序地層學理論，綜合利用地表露頭、鉆井巖芯、測井曲線資料和試氣成果資料，對鄂爾多斯盆地塔巴廟區塊晚古生代沉積體系及含氣層特徵進行了研究。結果表明，研究區內目的層段可以劃分為2個沉積體系： （ 1 ）上石炭統太原期為有障壁海岸沉積體系，發育潮坪?瀉湖?障壁砂壩沉積。 -
The measurement of the hydrochemistry mobility of the oil pollutant in the aeration zone
石油類污染物在包氣帶土層中的水化學遷移率測定 -
The movement of the water in aeration zone is different at different depth, if the zero flux potentials exist in the aeration zone
當包氣帶中存在零通量面時，包氣帶中水分的運移是分帶的。 -
For example, the salt capacity in the soil decreases with the increase of depth, while the lithology is the same in the aeration zone
在研究區，單一巖性的包氣帶中土壤的鹽份分佈自上到下是遞減的。 -
In the arid and semi - arid region, matrix potential of soil water diversifys intensively in aeration zone, so there is good environment for zero flux potentials to develop
結果表明：在干早和半乾旱地區，水土勢在包氣帶中變化強烈，具有良好的零通量面形成環境。 -
In the profile of aeration zone, the matrix potential of soil water and salt capacity in the soil can be affected by the lithology
即含水量大的地方的水土勢和土壤中總的含鹽量也大，含水量小的地方水土勢和土壤中總的含鹽量也小。 -
On studying of them. using the testing outcomes of gas fully, lithologic characters. strata sequence, sand body shape, sequence sectional structure in aeration zone and main channels migrating pattern on different phases have been analysed. for futher reservoir, cap, source rock and oil gas expiortion
在此研究基礎上，充分利用有關的試氣成果資料，詳細分析了含氣層的巖性、層序地層特點、砂體的形態產狀特徵、不同時期主河道分佈與遷移的規律及含氣層的剖面結構特點等。 -
The plants growing on the land surface can be affected by the occurrence and movement of water and salt in the aeration zone. in order to understand the characteristics of occurrence of water and salt in the aeration zone, we installed three tensionmeter systems. which includes 35 ceramic cups, in the soil of ejnqi oasis on the downstream of heihe river in inner mongolia province. the moisture potential distribution in aeration zone was observed, and the samples of water and soil were collected along the heihe river
為了了解綠洲包氣帶水分、鹽份的分佈特徵，我們在黑河下游的內蒙古額濟納旗綠洲安裝了3組35支負壓計，觀測包氣帶中的水土勢，並沿黑河河谷從下游的額濟納旗到中游的張掖採集土樣和水樣，測試土壤的易溶鹽和潛水的化學成分，從包氣帶中水土勢和鹽份兩個方面來研究乾旱地區水分和鹽份在包氣帶中賦存和運移規律。
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