Use of Rayleigh scatter for determining X-ray mass absorption coefficients.

A. H. Beavers, Kenneth R Olson

Research output: Contribution to journalArticle

Abstract

X-ray absorption is directly related to the atomic number of the element present and scatter is inversely related to the atomic number of the elements making up the sample. X-ray mass absorption coefficient can be used to characterize the homogeneity and changes of soil with depth. Each soil studied had a characteristic line expressing the relationship between mass absorption coefficient and soil depth. The maximum value appeared to reflect the maximum of soil mass including weathering productions such as clay, Fe, and bases. The subsoil tends to have a higher capacity to absorb X- rays than either the topsoil or parent material.-from Authors

Original languageEnglish (US)
Pages (from-to)1088-1091
Number of pages4
JournalSoil Science Society of America Journal
Volume50
Issue number4
DOIs
StatePublished - Jan 1 1986

Fingerprint

absorption coefficient
X-radiation
soil
parent material
subsoil
weathering
soil depth
topsoil
homogeneity
clay
sampling

ASJC Scopus subject areas

  • Soil Science

Cite this

Use of Rayleigh scatter for determining X-ray mass absorption coefficients. / Beavers, A. H.; Olson, Kenneth R.

In: Soil Science Society of America Journal, Vol. 50, No. 4, 01.01.1986, p. 1088-1091.

Research output: Contribution to journalArticle

@article{3d58d53b0d984df08d84f2a7651b384f,
title = "Use of Rayleigh scatter for determining X-ray mass absorption coefficients.",
abstract = "X-ray absorption is directly related to the atomic number of the element present and scatter is inversely related to the atomic number of the elements making up the sample. X-ray mass absorption coefficient can be used to characterize the homogeneity and changes of soil with depth. Each soil studied had a characteristic line expressing the relationship between mass absorption coefficient and soil depth. The maximum value appeared to reflect the maximum of soil mass including weathering productions such as clay, Fe, and bases. The subsoil tends to have a higher capacity to absorb X- rays than either the topsoil or parent material.-from Authors",
author = "Beavers, {A. H.} and Olson, {Kenneth R}",
year = "1986",
month = "1",
day = "1",
doi = "10.2136/sssaj1986.03615995005000040051x",
language = "English (US)",
volume = "50",
pages = "1088--1091",
journal = "Soil Science Society of America Journal",
issn = "0361-5995",
publisher = "Soil Science Society of America",
number = "4",

}

TY - JOUR

T1 - Use of Rayleigh scatter for determining X-ray mass absorption coefficients.

AU - Beavers, A. H.

AU - Olson, Kenneth R

PY - 1986/1/1

Y1 - 1986/1/1

N2 - X-ray absorption is directly related to the atomic number of the element present and scatter is inversely related to the atomic number of the elements making up the sample. X-ray mass absorption coefficient can be used to characterize the homogeneity and changes of soil with depth. Each soil studied had a characteristic line expressing the relationship between mass absorption coefficient and soil depth. The maximum value appeared to reflect the maximum of soil mass including weathering productions such as clay, Fe, and bases. The subsoil tends to have a higher capacity to absorb X- rays than either the topsoil or parent material.-from Authors

AB - X-ray absorption is directly related to the atomic number of the element present and scatter is inversely related to the atomic number of the elements making up the sample. X-ray mass absorption coefficient can be used to characterize the homogeneity and changes of soil with depth. Each soil studied had a characteristic line expressing the relationship between mass absorption coefficient and soil depth. The maximum value appeared to reflect the maximum of soil mass including weathering productions such as clay, Fe, and bases. The subsoil tends to have a higher capacity to absorb X- rays than either the topsoil or parent material.-from Authors

UR - http://www.scopus.com/inward/record.url?scp=0022928458&partnerID=8YFLogxK

UR - http://www.scopus.com/inward/citedby.url?scp=0022928458&partnerID=8YFLogxK

U2 - 10.2136/sssaj1986.03615995005000040051x

DO - 10.2136/sssaj1986.03615995005000040051x

M3 - Article

VL - 50

SP - 1088

EP - 1091

JO - Soil Science Society of America Journal

JF - Soil Science Society of America Journal

SN - 0361-5995

IS - 4

ER -