I~
~~
mt
2
we misht clisscsifty
Wd
way teens
~Vs4
this
plants
plus
Bate
tamale
the strontium,
ee
andeethon
rons
have the unavailal
ae
ius
4
ee
©
te
c
eet
ta
te
ri
te
SV
rye
~
the influcances
4.4
CG
1.
Wa Lind that the hisher the orsanie matt:
Q
4
ero,
“79
to es
find cut~ what
4
OQ
4
*
"
=
plus the organic
matto:
pietuve
CeCONES,.
Anothor study wa did was to take eig
-.
=
-
:
Bas on,
Dqek
-s- «VT.
wns
ane Leultuval soil tyros, inein vids
“ing one
from
Rutsers
UYJnivorsity,
Nevada and Now liexice soil,
In all cases, using these cvors,
again, we found that tho sassa
lation in the crops,
There are various ways that we misht ex-
‘plain this, but fT think it suis:
there is a very definite and a very significaat aditiference betwsen soils; and the more work we dd on thet aporoach, the
better, I think, we will unde2S tand the total picture,
'
[4
t.
{4
3
cr
ezficct of stadle stro
fs
dun itself--in other words, the
we plot activity accumulated in
the barley crop versus incronc nts of stabie strontium and
heen-
ing the activity in the soilec onstent in each interval here with
respect to stable, we find tha t the cunulation coeas tnis--it
increases as you increase the
for this, we get this sort of
wa
have the problen, and we ar