D Lal
Datos Biográficos
| ID | 5598601 |
|---|---|
| NOMBRE | D Lal |
| NOMBRES | D |
| APELLIDO | Lal |
| FIRMA | LAL D |
| AFILIACIONES | Fiji National University |
| ORCID | 0009-0002-4568-6301 |
| VERIFICADO | Sí |
| TOTAL DE OBRAS | 6 |
| TOTAL DE CITAS | 22 |
| TOTAL COMO AUTOR | 6 |
| TOTAL COMO EDITOR | 0 |
| PRIMER AÑO DE PUBLICACIÓN | 1963 |
| AÑO MÁS RECIENTE DE PUBLICACIÓN | 2023 |
| ÍNDICE H | 3 |
Ethics of care
Purpose The purpose of this paper is to explicate the links between public pedagogy, ethics of care and storying as a methodology and method in Oceania. Design/methodology/approach This paper explores the role of extended families as First Teachers in iTaukei and Indo-Fijian Early Childhood contexts in Fiji. Using storying as methodology, the authors, three Australian and four Fijian academics, present three portraits to make visible the pedagogi…
In-Situ Cosmogenic 14 C
Nuclear interactions of cosmic rays produce a number of stable and radioactive isotopes on the earth (Lai and Peters 1967). Two of these, 14 C and 10 Be, find applications as tracers in a wide variety of earth science problems by virtue of their special combination of attributes: 1) their source functions, 2) their half-lives, and 3) their chemical properties. The radioisotope, 14 C (half-life = 5730 yr) produced in the earth's atmosphere was the…
Cosmic ray labeling of erosion surfaces
Tata Institute Radiocarbon Date List III
In this paper are reported C 14 dates of archaeologic samples from the Neolithic, Harappan and Early Historic sites of India. C 14 activity was counted in an Oeschger-Houtermans’ gas proportional counter. The counting gas, acetylene, was synthesized using the technique described earlier (Kusumgar and others, 1963). The dates presented here are based on 5568 yr for the half-life of C 14 . The conversion to A.D./B.C. scale has been made using a.d. …
Tata Institute Radiocarbon Date List II
The C 14 dates presented here have been obtained by counting acetylene, synthesised from the sample, in an Oeschger-Houtermans’ gas proportional counter. The chemical and counting procedures have been described in some detail (Kusumgar et al. , 1963a). Dates are based on the C 14 half-life value of 5568 yr. For conversion of b.p. dates to a.d./b.c. scale, a.d. 1950 has been taken as the reference yr. Ninety-five % activity of NBS oxalic acid has …
Tata Institute Radiocarbon Date List I
The first series of C 14 dates obtained in the C 14 Laboratory of the above Institute, since it became operational in August 1961, are presented. The chemical and counting procedures adopted for the measurement of C 14 in our laboratory have been described in some detail (Kusumgar et al., 1962). For the sake of completeness some points relevant to the determination of dates are described below
Tata Institute Radiocarbon Date List I
The first series of C 14 dates obtained in the C 14 Laboratory of the above Institute, since it became operational in August 1961, are presented. The chemical and counting procedures adopted for the measurement of C 14 in our laboratory have been described in some detail (Kusumgar et al., 1962). For the sake of completeness some points relevant to the determination of dates are described below
Tata Institute Radiocarbon Date List III
In this paper are reported C 14 dates of archaeologic samples from the Neolithic, Harappan and Early Historic sites of India. C 14 activity was counted in an Oeschger-Houtermans’ gas proportional counter. The counting gas, acetylene, was synthesized using the technique described earlier (Kusumgar and others, 1963). The dates presented here are based on 5568 yr for the half-life of C 14 . The conversion to A.D./B.C. scale has been made using a.d. …
Tata Institute Radiocarbon Date List II
The C 14 dates presented here have been obtained by counting acetylene, synthesised from the sample, in an Oeschger-Houtermans’ gas proportional counter. The chemical and counting procedures have been described in some detail (Kusumgar et al. , 1963a). Dates are based on the C 14 half-life value of 5568 yr. For conversion of b.p. dates to a.d./b.c. scale, a.d. 1950 has been taken as the reference yr. Ninety-five % activity of NBS oxalic acid has …
In-Situ Cosmogenic 14 C
Nuclear interactions of cosmic rays produce a number of stable and radioactive isotopes on the earth (Lai and Peters 1967). Two of these, 14 C and 10 Be, find applications as tracers in a wide variety of earth science problems by virtue of their special combination of attributes: 1) their source functions, 2) their half-lives, and 3) their chemical properties. The radioisotope, 14 C (half-life = 5730 yr) produced in the earth's atmosphere was the…
Tata Institute Radiocarbon Date List I
The first series of C 14 dates obtained in the C 14 Laboratory of the above Institute, since it became operational in August 1961, are presented. The chemical and counting procedures adopted for the measurement of C 14 in our laboratory have been described in some detail (Kusumgar et al., 1962). For the sake of completeness some points relevant to the determination of dates are described below
Tata Institute Radiocarbon Date List II
The C 14 dates presented here have been obtained by counting acetylene, synthesised from the sample, in an Oeschger-Houtermans’ gas proportional counter. The chemical and counting procedures have been described in some detail (Kusumgar et al. , 1963a). Dates are based on the C 14 half-life value of 5568 yr. For conversion of b.p. dates to a.d./b.c. scale, a.d. 1950 has been taken as the reference yr. Ninety-five % activity of NBS oxalic acid has …
Tata Institute Radiocarbon Date List III
In this paper are reported C 14 dates of archaeologic samples from the Neolithic, Harappan and Early Historic sites of India. C 14 activity was counted in an Oeschger-Houtermans’ gas proportional counter. The counting gas, acetylene, was synthesized using the technique described earlier (Kusumgar and others, 1963). The dates presented here are based on 5568 yr for the half-life of C 14 . The conversion to A.D./B.C. scale has been made using a.d. …
Cosmic ray labeling of erosion surfaces
In-Situ Cosmogenic 14 C
Nuclear interactions of cosmic rays produce a number of stable and radioactive isotopes on the earth (Lai and Peters 1967). Two of these, 14 C and 10 Be, find applications as tracers in a wide variety of earth science problems by virtue of their special combination of attributes: 1) their source functions, 2) their half-lives, and 3) their chemical properties. The radioisotope, 14 C (half-life = 5730 yr) produced in the earth's atmosphere was the…
Ethics of care
Purpose The purpose of this paper is to explicate the links between public pedagogy, ethics of care and storying as a methodology and method in Oceania. Design/methodology/approach This paper explores the role of extended families as First Teachers in iTaukei and Indo-Fijian Early Childhood contexts in Fiji. Using storying as methodology, the authors, three Australian and four Fijian academics, present three portraits to make visible the pedagogi…
Geology (4 obras) · Radiocarbon dating (4 obras) · Chemistry (3 obras) · Environmental Science (3 obras) · Geography (3 obras) · Paleontology (3 obras) · Archaeology (2 obras) · Cosmic ray (2 obras) · Cosmogenic nuclide (2 obras) · Nuclear physics (2 obras)