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A Walton

Biographic Data

ID3643711
NAMEA Walton
GIVEN NAMESA
FAMILY NAMEWalton
SIGNATUREWALTON A
AFFILIATIONSLamont-Doherty Earth Observatory
VERIFIEDNo
TOTAL WORKS8
TOTAL CITATIONS27
AUTHOR COUNT8
EDITOR COUNT0
FIRST PUBLICATION YEAR1959
LATEST PUBLICATION YEAR2023
H-INDEX3
  • Resilience Measuring Tools for Risk Assessment & Disaster Preparedness in India

    Open Access•Tapaswini Mohapatra, Shailendra Mandal et al.•ARTICLE•International Society for the…•2023

    In today's increasingly complex and dynamic environment, the ability to manage environmental risks and seize opportunities for enhanced well-being is paramount for individuals, organizations, and governments. However, translating this concept into practice has proven to be a formidable challenge, primarily due to the absence of robust tools for the comprehensive assessment of resilience and its integration into development initiatives

  • Glasgow University Radiocarbon Measurements V

    Open Access•M Ergin, D D HARKNESS et al.•ARTICLE•Radiocarbon•1972•Cited by: 2•References: 4

    Operation of counting systems and preparation of results remain as described previously by Baxter et al. (1969), and Ergin et al. (1970)

  • Glasgow University Radiocarbon Measurements IV

    Open Access•D D HARKNESS, A Walton•ARTICLE•Radiocarbon•1972•Cited by: 3•References: 3

    The following list and data presented previously (R., 1970, v. 12, p. 494–495) were obtained to investigate the transport of carbon between man and his environment (Harkness, 1970). These data constitute a study of contemporary variations of C 14 concentrations viz. , Suess effect and bomb effect, as reflected in the tissues and food chain of the population of the United Kingdom (Harkness and Walton, 1969)

  • Glasgow University Radiocarbon Measurements III

    Open Access•M S Baxter, A Walton•ARTICLE•Radiocarbon•1970•Cited by: 5•References: 3

    The following list presents results obtained during 1968-69 on a series of samples chosen to investigate temporal variations of C 14 concentrations in the atmosphere during the past century. Together with data presented previously (Radiocarbon, 1969, v. 11, p. 45-52) they constitute a study of annual variations of C 14 activities at N temperate latitudes

  • Glasgow University Radiocarbon Measurements II

    Open Access•M Ergin, D D HARKNESS et al.•ARTICLE•Radiocarbon•1970•Cited by: 7•References: 3

    A third radiocarbon counting system has been established in the Chemistry Department, University of Glasgow, since April, 1968. Operating conditions for the previous systems have remained essentially as described by Baxter et al. (1969)

  • Glasgow University Radiocarbon Measurements I

    M S Baxter, M Ergin et al.•ARTICLE•Radiocarbon•1969•Cited by: 9•References: 9

    Two radiocarbon counting systems have been established in the Chemistry Department, University of Glasgow, since late 1967. The counting gas is methane, at pressures up to 10 atm, and 2 alternative procedures are followed for methane production, (a) high pressure synthesis in a stainless steel 4.5 1 reactor and (b) low pressure synthesis in an all glass flow-reactor. Both systems employ 0.5% ruthenium on alumina pellets as catalyst (Engelhard Ind…

  • Radioactive Dating and Methods of Low-level Counting

    Open Access•A Walton•ARTICLE•Antiquity•1967•Cited by: 1•References: 2

    An abstract is not available for this content so a preview has been provided. Please use the Get access link above for information on how to access this content

  • The geochemistry of C14 in fresh-water systems

    Open Access•Wallace S Broecker, A Walton•ARTICLE•Geochimica et Cosmochimica Acta•1959

  • Glasgow University Radiocarbon Measurements I

    M S Baxter, M Ergin et al.•ARTICLE•Radiocarbon•1969•Cited by: 9•References: 9

    Two radiocarbon counting systems have been established in the Chemistry Department, University of Glasgow, since late 1967. The counting gas is methane, at pressures up to 10 atm, and 2 alternative procedures are followed for methane production, (a) high pressure synthesis in a stainless steel 4.5 1 reactor and (b) low pressure synthesis in an all glass flow-reactor. Both systems employ 0.5% ruthenium on alumina pellets as catalyst (Engelhard Ind…

  • Glasgow University Radiocarbon Measurements II

    Open Access•M Ergin, D D HARKNESS et al.•ARTICLE•Radiocarbon•1970•Cited by: 7•References: 3

    A third radiocarbon counting system has been established in the Chemistry Department, University of Glasgow, since April, 1968. Operating conditions for the previous systems have remained essentially as described by Baxter et al. (1969)

  • Glasgow University Radiocarbon Measurements III

    Open Access•M S Baxter, A Walton•ARTICLE•Radiocarbon•1970•Cited by: 5•References: 3

    The following list presents results obtained during 1968-69 on a series of samples chosen to investigate temporal variations of C 14 concentrations in the atmosphere during the past century. Together with data presented previously (Radiocarbon, 1969, v. 11, p. 45-52) they constitute a study of annual variations of C 14 activities at N temperate latitudes

  • Glasgow University Radiocarbon Measurements IV

    Open Access•D D HARKNESS, A Walton•ARTICLE•Radiocarbon•1972•Cited by: 3•References: 3

    The following list and data presented previously (R., 1970, v. 12, p. 494–495) were obtained to investigate the transport of carbon between man and his environment (Harkness, 1970). These data constitute a study of contemporary variations of C 14 concentrations viz. , Suess effect and bomb effect, as reflected in the tissues and food chain of the population of the United Kingdom (Harkness and Walton, 1969)

  • Glasgow University Radiocarbon Measurements V

    Open Access•M Ergin, D D HARKNESS et al.•ARTICLE•Radiocarbon•1972•Cited by: 2•References: 4

    Operation of counting systems and preparation of results remain as described previously by Baxter et al. (1969), and Ergin et al. (1970)

  • Radioactive Dating and Methods of Low-level Counting

    Open Access•A Walton•ARTICLE•Antiquity•1967•Cited by: 1•References: 2

    An abstract is not available for this content so a preview has been provided. Please use the Get access link above for information on how to access this content

  • The geochemistry of C14 in fresh-water systems

    Open Access•Wallace S Broecker, A Walton•ARTICLE•Geochimica et Cosmochimica Acta•1959

  • Radioactive Dating and Methods of Low-level Counting

    Open Access•A Walton•ARTICLE•Antiquity•1967•Cited by: 1•References: 2

    An abstract is not available for this content so a preview has been provided. Please use the Get access link above for information on how to access this content

  • Glasgow University Radiocarbon Measurements I

    M S Baxter, M Ergin et al.•ARTICLE•Radiocarbon•1969•Cited by: 9•References: 9

    Two radiocarbon counting systems have been established in the Chemistry Department, University of Glasgow, since late 1967. The counting gas is methane, at pressures up to 10 atm, and 2 alternative procedures are followed for methane production, (a) high pressure synthesis in a stainless steel 4.5 1 reactor and (b) low pressure synthesis in an all glass flow-reactor. Both systems employ 0.5% ruthenium on alumina pellets as catalyst (Engelhard Ind…

  • Glasgow University Radiocarbon Measurements III

    Open Access•M S Baxter, A Walton•ARTICLE•Radiocarbon•1970•Cited by: 5•References: 3

    The following list presents results obtained during 1968-69 on a series of samples chosen to investigate temporal variations of C 14 concentrations in the atmosphere during the past century. Together with data presented previously (Radiocarbon, 1969, v. 11, p. 45-52) they constitute a study of annual variations of C 14 activities at N temperate latitudes

  • Glasgow University Radiocarbon Measurements II

    Open Access•M Ergin, D D HARKNESS et al.•ARTICLE•Radiocarbon•1970•Cited by: 7•References: 3

    A third radiocarbon counting system has been established in the Chemistry Department, University of Glasgow, since April, 1968. Operating conditions for the previous systems have remained essentially as described by Baxter et al. (1969)

  • Glasgow University Radiocarbon Measurements V

    Open Access•M Ergin, D D HARKNESS et al.•ARTICLE•Radiocarbon•1972•Cited by: 2•References: 4

    Operation of counting systems and preparation of results remain as described previously by Baxter et al. (1969), and Ergin et al. (1970)

  • Glasgow University Radiocarbon Measurements IV

    Open Access•D D HARKNESS, A Walton•ARTICLE•Radiocarbon•1972•Cited by: 3•References: 3

    The following list and data presented previously (R., 1970, v. 12, p. 494–495) were obtained to investigate the transport of carbon between man and his environment (Harkness, 1970). These data constitute a study of contemporary variations of C 14 concentrations viz. , Suess effect and bomb effect, as reflected in the tissues and food chain of the population of the United Kingdom (Harkness and Walton, 1969)

  • Resilience Measuring Tools for Risk Assessment & Disaster Preparedness in India

    Open Access•Tapaswini Mohapatra, Shailendra Mandal et al.•ARTICLE•International Society for the…•2023

    In today's increasingly complex and dynamic environment, the ability to manage environmental risks and seize opportunities for enhanced well-being is paramount for individuals, organizations, and governments. However, translating this concept into practice has proven to be a formidable challenge, primarily due to the absence of robust tools for the comprehensive assessment of resilience and its integration into development initiatives

Radiocarbon dating (6 works) · Archaeology (5 works) · Environmental Science (4 works) · Absolute dating (3 works) · Chemistry (3 works) · Geography (3 works) · Geology (3 works) · History (3 works) · Isotope Analysis in Ecology (3 works) · Archaeology and ancient environmental studies (2 works)

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