کد مقاله کد نشریه سال انتشار مقاله انگلیسی نسخه تمام متن
4675890 1634477 2012 7 صفحه PDF دانلود رایگان
عنوان انگلیسی مقاله ISI
Permittivity of ice at radio frequencies: Part II. Artificial and natural polycrystalline ice
موضوعات مرتبط
مهندسی و علوم پایه علوم زمین و سیارات علوم زمین و سیاره ای (عمومی)
پیش نمایش صفحه اول مقاله
Permittivity of ice at radio frequencies: Part II. Artificial and natural polycrystalline ice
چکیده انگلیسی

Precise knowledge of the absolute value and frequency dependence of the dielectric permittivity of ice is the basis for interpretation of radio echo sounding data on glaciers and ice sheets. However, in the range of radio-frequencies, data from direct measurements of the permittivity are sparse, and partially lacking uncertainty estimates. Here, we present new results for artificial and natural ice samples obtained by means of frequency-dependent measurements from 10 MHz to 1.5 GHz with a coaxial transmission line cell. Measurements on eight artificial ice samples grown from ultra-pure water within the cell yield a mean value for the real part of the relative permittivity of 3.18 ± 0.01 at − 20 °C. Sole evidence for dispersion is detected for frequencies below 10 MHz, possibly attributed to the Debye-type relaxation behavior. Investigation of the crystal orientation of the artificial ice samples reveals the c-axes to be predominantly parallel to the electric field inside the cell and allows to calculate a value representative for isotropic crystal orientation of 3.16 ± 0.01. Measurements on acid-doped artificial ice show a linear dependence of the real part with acidity with a gradient of (21.1 ± 3.9) [1/M]. The real part of the relative permittivity of natural firn and ice samples from a high Alpine glacier range from 2.02 at a density of 0.515 g/cm3 to 3.08 at 0.875 g/cm3. Quasi-continuous measurements with the present setup on an alpine firn core are now possible, with resolution depending on the coaxial cell's length, for direct comparison with the established dielectric profiling method.


► The real part of the permittivity of ice is measured at 1% uncertainty between 10 MHz and 1.5 GHz.
► The results show no signs of dispersion between 10 MHz and 1.5 GHz.
► In this range, measurements yield a mean value for the real part of isotropic ice of 3.16 +/− 0.01.
► Acid-doped ice and natural firn and ice samples were measured successfully.

ناشر
Database: Elsevier - ScienceDirect (ساینس دایرکت)
Journal: Cold Regions Science and Technology - Volumes 83–84, December 2012, Pages 13–19
نویسندگان
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