Abstract
Low-temperature nuclear orientation of 203Hg by electric quadrupole interaction has been observed in graphite intercalation compounds of HgCl 2. The measured electric field gradient V zz = −0.75(8) × 10 22 V m −2 is compared with the results on ion-implanted 203Hg samples and also with reported values in other intercalation compounds. Advantages and disadvantages of using intercalated samples, instead of ion-implanted samples, in nuclear orientation experiments are discussed.
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