規整嵌段 的英文怎麼說
中文拼音 [guīzhěngqiànduàn]
規整嵌段
英文
regular block-
But the design techniques of embedded system and embedded software is still germinant, and there are no integrated, standard and universal methods about it
但嵌入式系統以及嵌入式軟體設計技術仍舊處于起步階段，還未能形成一套完整、有效、通用的開發方法和規范。Embedded system is an application specific computer system that focuses on the application and it is based on the computer technologyjts hardware and software is cuttable. the development of embedded systems is very fast during the last ten years, furthermore, as an important part of embedded system, embedded operating system is uesed in the embedded systems more and more, especially in handheld devices and electronic devices. but the design techniques of embedded system and embedd software is still germinant, and there are no standards and universal methods about it
嵌入式系統是以應用為中心，以計算機技術為基礎，軟硬體可剪裁的專用計算機系統。近十幾年來，嵌入式系統的發展異常迅速，嵌入式操作系統作為嵌入式系統的核心，其應用也越來越廣泛，尤其在手持設備、信息家電領域更加突出。但嵌入式系統以及嵌入式軟體設計技術仍舊處于起步階段，仍舊未能形成一套完整、有效、通用的開發方法和規范。Meanwhile, most aspects about this perspective are concerned, which include quantification of the soil water background of the plateau area, the regional spatial variation of soil water background and variation along the slope, mosaic structure and seasonal changes etc. the results show that : ( 1 ) for the fundamental circumstance for vegetation development is the original debilitated slope, so the perspective of soil water background specially for the loess plateau refers to the soil water conditions on the original slope. ( 2 ) the value of soil water background appears to be a descending trend from south to north based on the difference of vegetation zones. in the forest zone, soil moisture contents beneath 3m depth from the soil surface are more than 12 % usually ; in the forest - pasture zone, the values of soil moisture content beneath 4m depth underground are more than 6 % and stable, and tend to be ascending while the depth increases ; but the values in the dry pasture zone is lingering between 4 % to 6 % from the surface layer to sub - layers
發展了「土壤水分背景」的概念，並以之為基礎對其各個方面進行了研究，使之形成一個相對獨立和完整的體系，主要包括黃土高原土壤水分的背景值、土壤水分背景的區域分異、坡面分異、鑲嵌結構及其季節分異等： （ 1 ）由於植被生長發展、演替的基礎階段是天然草被群落，故認為黃土高原的土壤水分背景在概念上是特指該區天然草被群落下的土壤水分狀況； （ 2 ）黃土高原的土壤水分背景值，根據植被地帶的不同表現出自南向北逐漸降低的規律：森林地帶3米以下土層水分背景值普遍穩定地高於12 ，森林草原地帶4米以下土層水分背景值穩定大於6 ，且均隨土層的加深水分含量逐漸增加，而草原帶的土壤水分背景值自土表至底土層一直在4 6之間徘徊。
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