Abstract
26
Al(r1/2 = 0.7 Ma), like
10
Be (r1/2 = 1.5 Ma), is produced by cosmic rays in the atm osphere, but its production rate is low (
ca
4 x 10
-3
that of
10
Be) and the crustal abundance o f
27
Al is high, resulting in
26
A1:27Al ratios rarely exceeding 10
~14
. Both isotopes are also produced in surficial rocks by cosmic rays; in quartz the production rates of
26
Al and
10
Be are
ca
. 70 atoms g
-1
a
-1
and
ca
. 10 atoms g
-1
a
-1
, respectively (at sea level). Because quartz frequently contains
27
Al at less than 100 p.p.m. (by mass), the
26
Al :
27
A1 ratio resulting from this situ production can be as high as 3 x 10
-11
. In extraterrestrial m atter, where the production rates are several hundred times greater, samples containing a few percent o f
27
Al have
26
Al:
27
Al ratios of 10
-11
or larger. We describe an experim ental arrangem ent that was developed at the University of Pennsylvania for measuring
26
A1:
27
Al ratios as low as 10-15. The size requirements for samples are approximately a factor of 100000 smaller than those of decay counting, and measurement times are less than an hour, compared with weeks or months. We discuss several applications of the technique to the measurement of terrestrial as well as extraterrestrial samples. Emphasis is placed on the combined measurement of
10
Be and
26
Al and the various uses to which the ratio o f
26
Al:
10
Be in a sample can be put. In particular, we discuss the very high
26
Al:
10
Be ratios that are found in the outer few millimetres of extraterrestrial bodies, resulting from low-energy protons emitted by solar flares, and the diagnostic value of these ratios in determining the size of objects in space. The low value of the
26
A1:
10
Be ratio resulting from atmospheric production is used to prove the terrestrial origin of tektites. And finally, we discuss the manner in which the variable
26
Al:
10
Be ratio that results from
in situ
production in objects on the Earth ’s surface can be used to measure rates of weathering and exposure histories.
Cited by
64 articles.
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