期刊
SCIENCE
卷 297, 期 5578, 页码 81-85出版社
AMER ASSOC ADVANCEMENT SCIENCE
DOI: 10.1126/science.1073722
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Using the Gamma-Ray Spectrometer on the Mars Odyssey, we have identified two regions near the poles that are enriched in hydrogen. The data indicate the presence of a subsurface layer enriched in hydrogen overlain by a hydrogen-poor layer. The thickness of the upper layer decreases with decreasing distance to the pole, ranging from a column density of about 150 grams per square centimeter at -42degrees latitude to about 40 grams per square centimeter at -77degrees. The hydrogen-rich regions correlate with regions of predicted ice stability. We suggest that the host of the hydrogen in the subsurface layer is ice, which constitutes 35 +/- 15% of the layer by weight.
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