soil

Chlorophyll-a Concentrations for Soil Biota Distribution Experiment

Abstract: 

 Investigation of the variation in soil biota and soil properties across the McMurdo Dry Valleys was part of the McMurdo Dry Valleys Long Term Ecological Research (LTER) project. Chlorophyll-a concentrations from soil samples collected for organism extraction and identification  was determined. Chlorophyll-a samples were gathered on the following dates:
 
 * December 12 and 22, 1994,
 * January 9, 1995,
 * November 8, 1995,
 * December 7, 1995, and
 * January 12, 1998. 
 

Dataset ID: 

237

Core Areas: 

Associated Personnel: 

582
583
584
585

Short name: 

gsca

Methods: 

 At each site 10-25 soil samples were taken for chlorophyll a analysis as follows:  Sampling bags were prepared with one sterile 'Whirlpak' bag and clean plastic scoop per sample.  The location of the sampling was recorded each year so that areas were not re-sampled.  Soil was collected to 1 cm depth with the plastic spoon, excluding rocks with a diameter >5 mm.  About 4 teaspoons of soil were placed into thevial, keeping the vial out of the light in a closed hand.  The soil samples were stored in a light-tight bag, in a cooler for transportation.  On return to the laboratory (within 8 hours of sampling), the soils were stored at +5 degrees C until further processing.
 
Extraction of chlorophyll from the soil. All procedures were carried out in the dark or very low irradiance to avoid degradation of the chlorophyll.  The soil samples were mixed thoroughly in the vials, and a sample of approximately 5 g was weighed out into a 50 mL plastic centrifuge tube with a screw-top cap. 10 mL of a 50:50 DMSO/90% acetone solution was added to each sample and they were mixed thoroughly on a bench-top Vortex mixer for about 5 seconds.  The vials were placed in a -4 degrees C constant temperature room, in the dark, and left for 12-18 hours.
 
Determination of chlorophyll-a concentration.  This was determined fluorometrically using a Turner model 111 fluorometer.  A calibration using a known concentration of chlorophyll was carried out prior to sample analysis. The machine was blanked using a 50:50 DMSO/90% acetone solution.  Each vial was mixed thoroughly, then centrifuged for 5 minutes at about 1800 RPM.  A sample of approximately 4 mL of the DMSO/acetone solution was taken from the top of the sample with a pipette, being careful not to get any soil particles in the solution.  The sample was placed in a cuvette, into the fluorometer and the fluorescence was recorded.  This was done fairly quickly in order to prevent light from breaking down the chlorophyll.  This measurement is called Fo, the initial fluorescence.  After taking this reading, 0.1 mL of 1N HCl was added directly to the cuvette and the cuvette was gently agitated.  After 20 seconds, the fluorescence was re-measured.  (During this step, the acid converts the chlorophyll to phaeophytin by releasing a magnesium ion in an acidic environment).  This measurement is called Fa, the fluorescence after acidification.  The solution was discarded into a waste container, and the cuvette rinsed 3 times with DMSO/90% acetone solution before proceeding with the next sample.  
 
Calculation of chlorophyll concentration.  The calibration curve that was constructed for the fluorometer had the following equation:  [chlorophyll (microg/L) = (Fo-Fa)-0.4254)/2.2385].  The Fo and Fa figures were put in to this equation to calculate chlorophyll concentration.  Subsequently, this figure was divided by 1000 to convert to microg/mL.  Next, this is multiplied by 10 as the soil was extracted in 10mL of DMSO/90% acetone.  Finally, this is divided by the fresh weight of the soil in g to give the concentration in microg chlorophyll per g fresh weight of soil.  If the extract was diluted prior to reading on the fluorometer, the dilution factor (noted in the comments column) was applied at the end of the equation.
 

Data sources: 

gsca

Maintenance: 

IN 2016, metadata was completed to enhance preservation, (San Gil) 
 
This file was created by Mark St. John at Colorado State University in Oct-1998, using raw data from the Excel workbooks '9412gsca.raw', '9511gsca.raw', and '9801gsca.raw'. The file format was suggested by the LTER data manager, to conform with the relational database structure. On 30-Oct-1998, the file was submitted to Denise Steigerwald, the MCM LTER data manager, located at INSTAAR, University of Colorado.
      
      Upon arrival at INSTAAR, the data manager combined the 3 data files, removed columns for latitude and longitude, and updated the location names to match those provided in the "soil measurement locations" file (from which latitude and longitude can be found). The resulting file was reformatted to present in ascii, comma delimited text and MS-DOS text (table layout) on the MCM LTER web site. Both of these files are linked to this web page above.  

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