کد مقاله کد نشریه سال انتشار مقاله انگلیسی نسخه تمام متن
1780950 1523924 2015 12 صفحه PDF دانلود رایگان
عنوان انگلیسی مقاله ISI
Martian airfall dust on smooth, inclined surfaces as observed on the Phoenix Mars Lander telltale mirror
ترجمه فارسی عنوان
گرد و غبار هواپیما مریخ بر روی سطح صاف و شیب دار مشاهده می شود که بر روی آینه فانیکس مریخ فرود می آید
موضوعات مرتبط
مهندسی و علوم پایه علوم زمین و سیارات فیزیک زمین (ژئو فیزیک)
چکیده انگلیسی


• Dust accumulation to one monolayer is fast and remains near constant over 150 sols.
• In contrast to past work, dust phase function is consistent with atmosphere at 450 nm.
• Phase function argues against size fractionation upon sedimentation.

The telltale mirror, a smooth inclined surface raised over 1 m above the deck of the Phoenix Mars Lander, was observed by the Surface Stereo Imager (SSI) several times per sol during the Phoenix Mars Lander mission. These observations were combined with a radiative transfer model to determine the thickness of dust on the wind telltale mirror as a function of time. 239 telltale sequences were analyzed and dustiness was determined on a diurnal and seasonal basis. The thickness of accumulated dust did not follow any particular diurnal or seasonal trend. The dust thickness on the mirror over the mission was 0.82±0.39 µm, which suggests a similar thickness to the modal scattering particle diameter. This suggests that inclining a surface beyond the angle of repose and polishing it to remove surface imperfections is an effective way to mitigate the accumulation of dust to less than a micron over a wide range of meteorological conditions and could be beneficial for surfaces which can tolerate some dust but not thick accumulations, such as solar panels. However, such a surface will not remain completely dust free through this action alone and mechanical or electrical clearing must be employed to remove adhered dust if a pristine surface is required. The single-scattering phase function of the dust on the mirror was consistent with the single-scattering phase function of martian aerosol dust at 450 nm, suggesting that this result is inconsistent with models of the atmosphere which require vertically or horizontally separated components or broad size distributions to explain the scattering behavior of these aerosols in the blue. The single-scattering behavior of the dust on the mirror is also consistent with Hapke modeling of spherical particles. The presence of a monolayer of particles would tend to support the spherical conclusion: such particles would be most strongly adhered electrostatically.

ناشر
Database: Elsevier - ScienceDirect (ساینس دایرکت)
Journal: Planetary and Space Science - Volume 116, October 2015, Pages 6–17
نویسندگان
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