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Commit 6f83b7df authored by mendrok's avatar mendrok
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* ARTS-XML-DATA-2-1-70

	* spectroscopy/Perrin/CO.xml.gz, HCl.xml.gz:
	Further corrections/updates.

	NOTE: previous updates of spectroscopic data (O2?) seem to have broken
	line mixing/zeeman test. Richard, please check (update reference values).

	* spectroscopy/Perrin/README: Updated accordingly.

	* planets/aux/isotopologue_ratios/isotopratios.py, isotopratios.txt:
	Minor improvements.



git-svn-id: https://radiativetransfer.org/svn/rt/arts-xml-data/trunk@8807 aaf1aab0-4228-0410-ad68-8dceda47f409
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2014-03-17 Jana Mendrok <jana.mendrok@ltu.se>
* ARTS-XML-DATA-2-1-70
* spectroscopy/Perrin/CO.xml.gz, HCl.xml.gz:
Further corrections/updates.
NOTE: previous updates of spectroscopic data (O2?) seem to have broken
line mixing/zeeman test. Richard, please check (update reference values).
* spectroscopy/Perrin/README: Updated accordingly.
* planets/aux/isotopologue_ratios/isotopratios.py, isotopratios.txt:
Minor improvements.
2014-03-07 Jana Mendrok <jana.mendrok@ltu.se>
* ARTS-XML-DATA-2-1-69
......
......@@ -82,12 +82,11 @@ def IRSingSpec(ir,st,en,tags,d):
print('N4/N5 from N2: %.3e' %dne)
#(1a) - 15N/14N
n = 2. #REPLACE permutational factor of N properly (equal the number of
#n = 1. #REPLACE permutational factor of N properly (equal the number of
# N-atoms that can be interchanged in position, e.g. 2 for N2)
# in case of only one pair of main-isotope-minor-isotope isotopologue we can
# derive internal isotopic ratio from
#miniso=-2 #common (if both H and N can be calculated)
#miniso=1 #if only N can be calculated, e.g. HNO3, N2
#dne = (1./n)*ir[miniso]/ir[0] #REPLACE indices properly
......@@ -114,11 +113,12 @@ def IRSingSpec(ir,st,en,tags,d):
dhp = dp[0,i]; dnp=dp[1,i]; rph = rp[0,i]; rpn = rp[1,i]
##### (E)
# REPLACE fac calc properly
#fac = N.ones(1) #when only the main isotopologue exists, e.g. C4H2
#fac = N.ones(1) #when only the main isotopologue exists, e.g. C4H2, PH3
#fac = N.append(N.ones(3),N.append(N.ones(3)*(dhp/dhe),(dhp/dhe)**2)) #H2O
#fac = N.append(1.,N.append(N.ones(2)*(dnp/dne),N.ones(2))) #N2O
#fac = N.append(N.ones(2),N.ones(2)*(dhp/dhe)) #CH4
#fac = N.append(1.,N.append((dnp/dne),(dhp/dhe))) #NH3
#fac = N.append(N.ones(2),N.append((dnp/dne),(dhp/dhe))) #HCN
#fac = N.append(1.,(dnp/dne)) #HNO3, N2
#fac = N.append(N.ones(2),N.ones(2)*(dhp/dhe)) #HBr,HCl
fac = N.append(1.,(dhp/dhe)) #HI,HF,H2
......
......@@ -51,14 +51,14 @@ Isotopologue ratio is the product of the relative isotopic abundances of all
example:
IR(CH4) = ia(C) * ia(H)**4 #1C atom, 4H
IR(CH3D) = ia(C) * ia(H)**3 * ia(D) * 4 #1C atom, 3H aoms, 1D atom
IR(CH3D) has a factor 4 since D can be in place of any of the 4H, i.e. for us
IR(CH3D) has a factor 4 since D can be in place of any of the 4H, i.e., for us
CH3D stands for CHHHD and CHHDH and CHDHH and CDHHH, hence their abundances
have to be summed up.
The isotopic abundance ia can be expressed in terms of the isotopic ratios ir
(i.e., abundance of an isotope in relation to the main or another isotope):
ia = ir(i) / (sum_j=1^N ir(j)
i.e. as the relation of the individual isotope's abundance in relation to a
ia(i) = ir(i) / ( sum_j=1^N ir(j) )
i.e., as the relation of the individual isotope's abundance in relation to a
fixed (usually the main) isotope to the sum of the relative abundances of all
isotopes to the fixed (main) isotope.
......
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......@@ -58,20 +58,20 @@ Latest version:
Nov 23 2012 C3H8.xml.gz
Mar 15 2012 CH4.xml.gz
Mar 1 2012 CO.xml.gz
Mar 17 2014 CO.xml.gz
Jan 29 2014 CO2.xml.gz
Mar 1 2012 H2CO.xml.gz
Jan 29 2014 H2O.xml.gz
Mar 15 2012 H2O2.xml.gz
Mar 1 2014 H2S.xml.gz
Mar 15 2012 H2SO4.xml.gz
Feb 17 2014 HCl.xml.gz
Feb 17 2014 HF.xml.gz
Mar 17 2014 HCl.xml.gz
Mar 1 2014 HF.xml.gz
Aug 23 2012 HO2.xml.gz
Mar 15 2012 NH3.xml.gz
Feb 6 2014 O2.xml.gz
Feb 6 2014 O3.xml.gz
Feb 17 2014 OCS.xml.gz
Mar 1 2014 OCS.xml.gz
Mar 15 2012 PH3.xml.gz
Mar 19 2012 SO.xml.gz
Feb 6 2014 SO2.xml.gz
......
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