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Scientific and Technical Aerospace Reports Volume 39 April 6, 2001

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tions of water. Often, due to lower temperatures coupled with the superior insulation properties of the surrounding rock, these<br />

accumulations are in the form of ice. Historically, ice was mined from some lava tube caves. Many of the lava tubes in the Central<br />

Oregon area sport such names as ”Arnolds Ice Cave,” ”Surveyors Ice Cave,” ”South Ice Cave,” etc. These caves are not caves<br />

in ice, but rather common lava tubes with seasonal, <strong>and</strong> sometimes perennial ice deposits. Locating <strong>and</strong> cataloging similar features<br />

on Mars, could be of value for the colonization of Mars <strong>and</strong> the search for life. Such features may also prove useful in helping<br />

to determine past climatic conditions on the Red Planet.<br />

Derived from text<br />

Mars (Planet); Caves; Ice; Planetary Geology<br />

<strong>2001</strong>0023106 NASA Ames Research Center, Moffett Field, CA USA<br />

Mars Oxidant: Proof of Concept <strong>and</strong> Quantitative Analysis<br />

Freund, Friedemann, NASA Ames Research Center, USA; Staple, Aaron, Stanford Univ., USA; Gosling, Paul, San Jose State<br />

Univ., USA; Belisle, Warren, Lockheed Martin Engineering <strong>and</strong> Science Services, USA; Concepts <strong>and</strong> Approaches for Mars<br />

Exploration; July 2000, Part 1, pp. 116-117; In English; See also <strong>2001</strong>0023036; No Copyright; Avail: CASI; A01, Hardcopy; A03,<br />

Microfiche<br />

Textbooks make us believe that in every silicate mineral, on Earth, Mars <strong>and</strong> elsewhere, the oxygen anions exist in just one<br />

oxidation state, namely 2(-) as in 0(-2). Yet, a surprisingly large fraction of the oxygen anions in rock-forming minerals may exist<br />

in a more oxidized form, namely the 1- state, as 0(-) in peroxy. This has far-reaching consequences for underst<strong>and</strong>ing the Mars<br />

soil oxidant <strong>and</strong> its biocompatibility.<br />

Derived from text<br />

Mars Surface; Biocompatibility; Quantitative Analysis; Anions; Oxygen<br />

<strong>2001</strong>0023107 Planetary Society, Pasadena, CA USA<br />

Connecting Robots <strong>and</strong> Humans in Mars Exploration<br />

Friedman, Louis, Planetary Society, USA; Concepts <strong>and</strong> Approaches for Mars Exploration; July 2000, Part 1, pp. 118; In English;<br />

See also <strong>2001</strong>0023036; No Copyright; Avail: CASI; A01, Hardcopy; A03, Microfiche<br />

Mars exploration is a very special public interest. It’s preeminence in the national space policy calling for ”sustained robotic<br />

presence on the surface,” international space policy (witness the now aborted international plan for sample return, <strong>and</strong> also aborted<br />

Russian ”national Mars program”) <strong>and</strong> the media attention to Mars exploration are two manifestations of that interest. Among<br />

a large segment of the public there is an implicit (mis)underst<strong>and</strong>ing that we are sending humans to Mars. Even among those who<br />

know that isn’t already a national or international policy, many think it is the next human exploration goal. At the same time the<br />

resources for Mars exploration in the U.S. <strong>and</strong> other country’s space programs are a very small part of space budgets. Very little<br />

is being applied to direct preparations for human flight. This was true before the 1999 mission losses in the USA, <strong>and</strong> it is more<br />

true today. The author’s thesis is that the public interest <strong>and</strong> the space program response to Mars exploration are inconsistent. This<br />

inconsistency probably results from an explicit space policy contradiction: Mars exploration is popular because of the implicit<br />

pull of Mars as the target for human exploration, but no synergy is permitted between the human <strong>and</strong> robotic programs to carry<br />

out the program. It is not permitted because of narrow, political thinking. In this paper we try to lay out the case for overcoming<br />

that thinking, even while not committing to any premature political initiative. This paper sets out a rationale for Mars exploration<br />

<strong>and</strong> uses it to then define recommended elements of the programs: missions, science objectives, technology. That consideration<br />

is broader than the immediate issue of recovering from the failures of Mars Climate OrbIter, Mars Polar L<strong>and</strong>er <strong>and</strong> the Deep Space<br />

2 microprobes in late 1999. But we cannot ignore those failures. They are causing a slow down Mars exploration. Not only were<br />

the three missions lost, with their planned science <strong>and</strong> technology investigations, but the <strong>2001</strong> Mars Surveyor l<strong>and</strong>er; <strong>and</strong> an international<br />

cooperative effort for robotic Mars sample return were also lost.<br />

Derived from text<br />

Mars Exploration; Public Relations; Mars Missions<br />

<strong>2001</strong>0023108 Planetary Society, Pasadena, CA USA<br />

Public Participation in Planetary Exploration<br />

Friedman, Louis, Planetary Society, USA; Concepts <strong>and</strong> Approaches for Mars Exploration; July 2000, Part 1, pp. 119; In English;<br />

See also <strong>2001</strong>0023036; No Copyright; Abstract Only; Available from CASI only as part of the entire parent document<br />

In the past several years The Planetary Society has created several innovative opportunities for general public participation<br />

in the exploration of the solar system <strong>and</strong> the search for extraterrestrial life. The conduct of such exploration has traditionally been<br />

the province of a few thous<strong>and</strong>, at most, of professionally involved scientists <strong>and</strong> engineers. Yet the rationale for spending<br />

resources required by broad <strong>and</strong> far-reaching exploration involves a greater societal interest - it frequently being noted that the<br />

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