Title: DIELECTRIC MEASUREMENTS USING A VECTOR NETWORK ANALYZER FOR GREENLAND AND ANTARCTICA ICE CORE SAMPLES Tyler L. Berry, Fernando Rodriguez-Morales, Stephen Yan, CReSIS, University of Kansas, Lawrence KS 66045, Haskell Indian Nations University, Lawrence
1DIELECTRIC MEASUREMENTS USING A VECTOR NETWORK
ANALYZER FOR GREENLAND AND ANTARCTICA ICE CORE
SAMPLESTyler L. Berry, Fernando
Rodriguez-Morales, Stephen Yan, CReSIS,
University of Kansas, Lawrence KS 66045, Haskell
Indian Nations University, Lawrence KS 66046
- Abstract
- Sea level is strongly linked to the growth and
shrinkage of the large ice sheets in Greenland
and Antarctica. There is an urgent need to
improve both knowledge of ice dynamics and
accuracy of ice-sheet models to predict the
ice-sheets response to a warming climate and
their contribution to sea level rise. A key
component to improve the ice sheet models through
the use and interpretation of radar data is the
knowledge of the dielectric properties of the
ice. Most of the measured data on the dielectric
properties of ice available today is based on
measurements performed at low frequencies with
the technology available in the 1960s and again
in the 80s. In this project we will design and
fabricate a set of test fixtures to characterize
relative permittivity of dielectric materials
using a vector network analyzer. One technique to
be used relies on a planar transmission line in
contact with the sample, where the sample acts as
a dielectric loading to the line. By measuring
the change in the transmission and reflection
coefficients of the transmission line, the
relative permittivity of the sample can be
retrieved. The method will serve as a basis for
dielectric measurements on dielectric materials
in the 10-1000 MHz range and will be used as a
test bench for future measurements on ice cores.
Construction of a Test Bed for Ice Core
Measurement
- Methodology
- The first step was to determine a suitable
material to create the test stand out of and for
its dielectric properties to not interfere with
the measurements of the ice cores. The dielectric
constant needed to be less than 3.0 but it would
be more beneficial to be closer to 2.0. We could
get a rough estimate of materials dielectric
constants from tables researched on the internet.
The results had tolerances on some materials too
wide to make a good estimate on whether they were
suitable. - Samples of materials were ordered that had a
price range suitable for our purposes and then
prepared to test their dielectric constants. - Copper tape was covered on one side of the
material and a 3/8 inch strip of copper tape
placed down the center on the reverse side (Fig.
1 and 2). - A PCB Endlaunch SMA .042 inch Connector was then
soldered to the sample. The center pin of the SMA
was soldered to the 3/8 inch strip and the outer
conductor of the SMA was then soldered to the
completely covered side (Fig. 3 and 4). - The information gathered from the Network
Analyzer was transferred to the Agilent Advanced
Design System program (ADS) on a computer and the
dielectric constant of the material was derived. - The results of the High Density Polyethylene
(HDPE) (2.16) and the price of materials were
satisfactory to our purpose and it was decided to
use this material for our platform. - The design in SolidWorks Computer Animated
Design (CAD) was determined after the material
was selected. The design was determined based on
material characteristics and material size that
could be purchased.
Conclusion Further testing is required after the
construction of the test platform to determine if
the material and dimensions will be sufficient.
Test samples will be used in substitution of the
ice cores to see how it well it employs the
return data. After final testing we will use the
measured dielectric data of the ice cores to
simulate radar returns at existing core sites and
compare these returns with experimental results.
We will perform measurements of existing ice
cores in collaboration with Prof. Dorthe
Dahl-Jensen and her team at the University of
Copenhagen. After verifying the performance of
the probe, we will convert the system to perform
measurements in the field on new cores to be
drilled.
Purpose To develop and demonstrate a system for
dielectric measurements in the frequency range of
10-1000 MHz. This system will consist of a
coplanar waveguide test platform (See Test
Platform Model). An ice core sample can be place
on the platform and impedance measurements can be
performed with a vector analyzer. The test
platform will allow characterization of the
samples without further cutting or slicing of the
ice core sample. With the accurate ice
core-derived DEP from the new measurement system,
we can invert existing radar data as well as the
new ultrawideband radar depth sounder (150-600
MHz) that is currently under development by
CReSIS (deployment planned for winter 2013) to
unambiguously determine the basal conditions over
many areas of the Ice Sheets in Greenland and
Antarctica.
References WCRP, Understanding sea-level rise
and variability, Workshop Report. IOC/UNESCO,
Paris, France, June 6-9, 2006. Dahl-Jensen, D.
et al., Eemain interglacial reconstructed from a
Greenland folded ice core, Nature, vol. 493, pp.
489-494, 2013. Van der Veen, C.J. and ISMASS
Members, A Need for More Realistic Ice-Sheet
Models, SCAR Report No.30, 2007. Evans, S.,
Dielectric properties of ice and snow a
review, Journal of Glaciology, vol. 5, no. 42,
pp. 773-792, 1965. Fujita, S., Shiraishi, M.,
and Mae, S., Measurement on the dielectric
properties of acid-doped ice at 9.7 GHz, IEEE
Transactions on Geoscience and Remote Sensing,
vol. 30, no. 4, pp. 799-803, 1992. Wilhelms, F.,
et al., Precise dielectric profiling of ice
cores a new device with improved guarding and
its theory, Journal of Glaciology, vol. 44, no.
146, pp. 171-174, 1998. Havrilla, M. J., and
Nyquist, D. P., Electromagnetic characterization
of layered materials via direct and de-embed
methods, IEEE Transactions on Instrumentation
and Measurement, vol. 55, no. 1, pp. 158-163,
2006.
General Estimation Procedure
ADS Simulated and Tested Results