Skip Navigational Links
LISTSERV email list manager
LISTSERV - LIST.UVM.EDU
LISTSERV Menu
Log In
Log In
LISTSERV 17.5 Help - ISOGEOCHEM Archives
LISTSERV Archives
LISTSERV Archives
Search Archives
Search Archives
Register
Register
Log In
Log In

ISOGEOCHEM Archives

Stable Isotope Geochemistry

ISOGEOCHEM@LIST.UVM.EDU

Menu
LISTSERV Archives LISTSERV Archives
ISOGEOCHEM Home ISOGEOCHEM Home

Log In Log In
Register Register

Subscribe or Unsubscribe Subscribe or Unsubscribe

Search Archives Search Archives
Options: Use Forum View

Use Monospaced Font
Show Text Part by Default
Show All Mail Headers

Message: [<< First] [< Prev] [Next >] [Last >>]
Topic: [<< First] [< Prev] [Next >] [Last >>]
Author: [<< First] [< Prev] [Next >] [Last >>]

Print Reply
Subject:
Re: Three source mixing model
From:
Jonathan Wynn <[log in to unmask]>
Reply To:
Stable Isotope Geochemistry <[log in to unmask]>
Date:
Thu, 27 Jul 2006 10:52:45 -0400
Content-Type:
text/plain
Parts/Attachments:
text/plain (63 lines)
Jude,

Assuming you do not accurately know the concentration and isotopic  
composition of carbonate in your samples (if it varies between  
samples), you may not be able to apply a three component isotope mass  
balance to solve for your two unknowns.

Have you considered simply removing the carbonate prior to (re-) 
analysis by EA-MS?  If there is remaining sample, they can be acid- 
treated in silver capsules.  There is a lot of discussion of this  
topic on ISOGEOCHEM under carbonate removal.  One most useful  
methodological reference is:

Verardo, D.J, P.N. Froelich, and A. McIntyre, 1990, Determination of  
organic carbon and nitrogen in marine sediments using the Carlo Erba  
NA-1500 Analyzer, Deep Sea Research, Vol. 37, No.1, 157-165.

Best,

Jonathan Wynn
Department of Geology
University of South Florida
4202 E Fowler Ave, SCA 528
Tampa, FL 33620
(813) 974-9369
[log in to unmask]
http:shell.cas.usf.edu/~jwynn



On Jul 26, 2006, at 6:57 PM, judemaul wrote:

> Folks,
>
> I am characterizing particulate plant derived organic matter input  
> to the soil.  The approach I have taken is planting C3 plants into  
> a soil with a long C4 history.  The particulate organic matter in  
> the soil at the start of the experiment had a del vPDB signature of  
> -14.000 and the new C3 input has a del vPDB of -28.000.  My problem  
> is that the protocol for isolating the organic matter requires that  
> I co-collect the organic matter with the sand fraction of the soil,  
> which contains about 18% carbonate with a del vPDB of 0. I'm  
> wondering if anybody can help me with a three source mixing model  
> that can be run using only one isotope?  Using a separate analysis  
> of the soil I can calculate the amount of carbonate in each sample  
> but I need to determine the proportion of each plant source (C3 or  
> C4) in the remaining organic carbon.
> Ideally I would have removed the carbonate prior to isotopic  
> analysis but at the time of sample prep I didn't realize how much  
> of an issue the carbonate would be.
>
> Thanks
> jude
>
> -- 
> ####################
> Jude Maul
> Department of Horticulture
> Cornell University
> [log in to unmask]
> (607)255-0883 (office)
> ####################

ATOM RSS1 RSS2

LIST.UVM.EDU CataList Email List Search Powered by LISTSERV