scholarly journals Further history of a quartz thread gravity balance

A former paper* by one of the present authors and JAMES ARTHUR POLLOCK contains an account of the construction of a quartz thread gravity balance which was made at the University of Sydney during the time R. THRELFALL was Professor of Physics there. This work extended from 1889 up to the time of publication, and included an account of a good many gravimetric observations at Sydney, Melbourne, Hobart, and at various places in New South Wales. Final tests were made by taking the balance to and fro between Sydney and Hornsby, which is near Sydney but is 592 feet above sea-level, the University of Sydney, which was the Sydney observation station, being only slightly above sea-level (120 feet). As the result of several such journeys we finally felt entitled to say that “ We have therefore determined the value of g at Hornsby relatively to that at Sydney in three journeys with a maximum difference of 0.4 sextant minutes, or to less than 1 part in 500,000 in the value of g ." It had been intended to embark on a series of observations on the Australian coast, but, unfortunately, R. THRELFALL returned to England in 1898 and arrangements for carrying on the work had to be considered. J. A. POLLOCK succeeded R. THRELFALL as Professor of Physics at the Sydney University, and it was arranged that the balance, which, by the way, had been exhibited at the British Association Meeting at Dover, should be in J. A. POLLOCK’s charge and that he should continue the work in so far as his new duties as Professor of Physics enabled him to do so. Unfortunately, an opportunity never occurred and the balance was stored in one of the cellars of the Physical Laboratory of the University till 1923. Meanwhile Professor POLLOCK died.

PEDIATRICS ◽  
1964 ◽  
Vol 33 (5) ◽  
pp. 805-805
Author(s):  
CLEMENT A. SMITH

For the pediatrician curious enough to pursue the life history of his patient into its prenatal phase or the obstetrician interested in more than one of his two patients, this small book will be of great usefulness. Of the twenty-one chapters, twelve are by Australian or New Zealand workers, the Editor, a Professor of Obstetrics and Gynaecology at the University of New South Wales, among them. The international flavor is augmented by Swedish, German, and Scottish contributors.


2017 ◽  
Vol 65 (3) ◽  
pp. 165 ◽  
Author(s):  
Lyn S. Nelson ◽  
Paul D. Cooper

The endangered grassland earless dragon, Tympanocryptis pinguicolla, is present in two geographic locations in Australia: the Australian Capital Territory and adjacent New South Wales (NSW) near Canberra (~580 m above sea level) and Monaro Plains, NSW, near Cooma (~950 m above sea level). The lizards live in native grassland, an endangered ecological community, and although the population ecology of the animal has been examined, the importance of habitat for thermoregulatory patterns is unknown. We studied whether lizards from the two locations differ in their seasonal patterns of thermoregulation by measuring skin and chest temperatures using both radio-telemetry and temperature measurement in the field, as well as thermal preferences in a laboratory thermal gradient. These results are compared with the operative temperatures (Te) in various microhabitats in the two regions to determine to what extent lizards are thermoregulating. We demonstrate that these lizards do not maintain a constant body temperature, but allow Tb to vary between 13 and 39°C when active in the field, although the grand mean for 50% basking temperatures ranged between 32 and 36°C in the laboratory gradient. Temperatures in the various microhabitats can exceed 40°C, but lizards appeared to avoid those temperatures by seeking shelter in either burrows or the base of grass tussocks. Lizards could choose microhabitats that would permit maintenance of body temperatures above 30°C in most seasons, but did not do so. As high body temperature is not selected in field conditions for either population, other processes (e.g. predation) may be more important for determining Tb maintenance.


1992 ◽  
Vol 38 (3) ◽  
pp. 347-358 ◽  
Author(s):  
Andrew McMinn

AbstractThe Richmond River Valley of northern N.S.W. contains a late Pleistocene succession dating back to approximately 250,000 yr B.P. Dinoflagellate and spore-pollen assemblages from the lowest interval, the lower “Dungarubba Clay” of Drury (1982), indicate deposition in a restricted estuarine environment at approximately 250,000 yr. Deposition in the overlying interval, the upper “Dungarubba Clay” and “Gundurimba Clay”, at approximately 120,000 yr B.P., began in a restricted estuary, but rising sea level caused inundation and deposition in a more open, marine-dominated environment. Dinoflagellate cyst assemblages from the last interglaciation (stage 5) are interpreted by analogy with those from the morphologically similar, modern Broken Bay, N.S.W. They are indicative of an open, marine-dominated environment and imply that barrier formation in the Richmond River Valley, and possibly elsewhere in northern N.S.W., did not commence until after the initial postglacial transgression. Synchronous changes in sea level and rainforest development suggest that there was no significant time lag between climate and sea-level change.


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