翻訳と辞書 Words near each other ・ Barolo Boys ・ Barolo shearwater ・ Barolo, Piedmont ・ Barolong Seboni ・ Barom Reameathibtei ・ Barom-1 ・ Baromesnil ・ Barometer ・ Barometer (sculpture) ・ Barometer Clock ・ Barometer question ・ Barometer Rising ・ Barometer Soup ・ Barometer World ・ Barometern ・ Barometric formula ・ Barometric light ・ BARON ・ Baron ・ Baron & Budd asbestos memo ・ Baron & Budd, P.C. ・ Baron (disambiguation) ・ Baron (name) ・ Baron (photographer) ・ Baron 1898 ・ Baron Aberconway ・ Baron Abercromby ・ Baron Aberdare ・ Baron Abinger ・ Baron Acton Dictionary Lists mini英和辞書 mini和英辞書 Webster 1913 Latin-English FOLDOC Wikipedia English ウィキペディア

翻訳と辞書　辞書検索 [ 開発暫定版 ] スポンサード リンク Barometric formula ： ウィキペディア英語版 Barometric formula The barometric formula, sometimes called the ''exponential atmosphere'' or ''isothermal atmosphere'', is a formula used to model how the pressure (or density) of the air changes with altitude. ==Pressure equations== There are two different equations for computing pressure at various height regimes below 86 km (or 278,400 feet). The first equation is used when the value of standard temperature lapse rate is not equal to zero; the second equation is used when standard temperature lapse rate equals zero. Equation 1: : where :$P\_b$ = static pressure (pascals) :$T\_b$ = standard temperature (K) :$L\_b$ = standard temperature lapse rate (K/m) in ISA :$h$ = height above sea level (meters) :$h\_b$ = height at bottom of layer ''b'' (meters; e.g., ''h1'' = 11,000 meters) :$R^$ * = universal gas constant for air: 8.31432 N·m /(mol·K) :$g\_0$ = gravitational acceleration (9.80665 m/s2) :$M$ = molar mass of Earth's air (0.0289644 kg/mol) Or converted to imperial units:〔Mechtly, E. A., 1973: ''The International System of Units, Physical Constants and Conversion Factors''. NASA SP-7012, Second Revision, National Aeronautics and Space Administration, Washington, D.C.〕 where :$P\_b$ = static pressure (inches of mercury, inHg) :$T\_b$ = standard temperature (K) :$L\_b$ = standard temperature lapse rate (K/ft) in ISA :$h$ = height above sea level (ft) :$h\_b$ = height at bottom of layer ''b'' (feet; e.g., ''h1'' = 36,089 ft) :$R^$ * = universal gas constant; using feet, kelvins, and (SI) moles: 8.9494596×104 lb·ft2/(lb-mol·K·s2) :$g\_0$ = gravitational acceleration (32.17405 ft/s2) :$M$ = molar mass of Earth's air (28.9644 lb/lb-mol) The value of subscript ''b'' ranges from 0 to 6 in accordance with each of seven successive layers of the atmosphere shown in the table below. In these equations, ''g''0, ''M'' and ''R'' * are each single-valued constants, while ''P,'' ''L,'' ''T,'' and ''h'' are multivalued constants in accordance with the table below. The values used for ''M,'' ''g''0, and ''R'' * are in accordance with the U.S. Standard Atmosphere, 1976, and the value for ''R'' * in particular does not agree with standard values for this constant.〔(U.S. Standard Atmosphere ), 1976, U.S. Government Printing Office, Washington, D.C., 1976. (Linked file is 17 Mb)〕 The reference value for ''Pb'' for ''b'' = 0 is the defined sea level value, ''P0'' = 101325 pascals or 29.92126 inHg. Values of ''Pb'' of ''b'' = 1 through ''b'' = 6 are obtained from the application of the appropriate member of the pair equations 1 and 2 for the case when ''h = hb+1''.〔 抄文引用元・出典: フリー百科事典『 ウィキペディア（Wikipedia）』 ■ウィキペディアで「Barometric formula」の詳細全文を読む スポンサード リンク 翻訳と辞書 : 翻訳のためのインターネットリソース Copyright(C) kotoba.ne.jp 1997-2016. All Rights Reserved.