The superparamagnetism of Yucca Mountain Tuff

被引:119
|
作者
Worm, HU [1 ]
Jackson, M
机构
[1] Fed Inst Geosci & Nat Resources, D-3000 Hannover, Germany
[2] Univ Minnesota, Sch Earth Sci, Inst Rock Magnetism, Minneapolis, MN 55455 USA
关键词
D O I
10.1029/1999JB900285
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
Yucca Mountain Tuff contains small titanomagnetite grains with narrow size distributions in the superparamagnetic range [Schlinger et al., 1988]. Magnetic measurements on three samples (comprising hysteresis loops at low and ambient temperatures, acquisition and demagnetization of isothermal remanent magnetization, thermal demagnetization of the saturation remanence and of a low-temperature thermoremanence, and frequency- and temperature-dependent susceptibilities) allow evaluation of the magnetic properties in terms of Neel's [1949] single-domain theory. Precise grain volume distributions have been obtained by applying the blocking volume concept to thermal demagnetization results. In contrast, an attempt to derive mean particle volumes by fitting a Langevin curve to the room temperature magnetization curves fails, probably because the precondition for the Langevin function, KV/kT << 1, is not met. It is only for the sample with the smallest grains and in weak fields (< 20 mT) that a Langevin fit provides a reasonable volume estimate. There is good agreement between the experimental results and the calculated frequency and temperature dependence of susceptibility, thus verifying that Neel's theory is sufficient for the magnetic description of single-domain assemblages spanning the superparamagnetic/stable single-domain boundary. However, some deviations between modeled and measured susceptibilities exist, and the physical causes may include size-dependent anisotropy, nonuniform magnetizations, and also an uncertain preexponential time "constant" tau(o). While tau(o) = 10(-11) s gives the best fit for the sample with the largest grains, tau(o) = 10(-9) s is more reasonable for the others. Thus tau(o) may indeed be size- and temperature-dependent as predicted by Brown [1959]. The commonly cited parameter chi(fd) (frequency dependence of susceptibility) reaches 30% at room temperature (RT) for one sample with a blocking temperatures just below RT, while chi(fd) = 0 at RT for a superparamagnetic sample with smaller grains. These results thus exemplify that chi(fd) is not limited to 15%, as a number of studies suggest, and that chi(fd) = 0 must not be taken to imply the absence of superparamagnetic grains.
引用
收藏
页码:25415 / 25425
页数:11
相关论文
共 50 条
  • [1] Sorption of neptunium and plutonium to Yucca Mountain tuff
    Sullens, Tyler A.
    Daniels, Jeanette
    Czerwinski, Ken
    ABSTRACTS OF PAPERS OF THE AMERICAN CHEMICAL SOCIETY, 2007, 233
  • [2] The effect of saturation on the mechanical properties of tuff at Yucca Mountain
    Karakouzian, M
    Hudyma, N
    HIGH LEVEL RADIOACTIVE WASTE MANAGEMENT, 1996 ., 1996, : 407 - 408
  • [3] SORPTION ISOTHERMS AND MATRIX DIFFUSION IN YUCCA MOUNTAIN TUFF
    RUNDBERG, RS
    KNIGHT, SJ
    THOMPSON, JL
    ABSTRACTS OF PAPERS OF THE AMERICAN CHEMICAL SOCIETY, 1982, 183 (MAR): : 33 - NUCL
  • [4] PYRITIC ASH-FLOW TUFF, YUCCA MOUNTAIN, NEVADA
    CASTOR, SB
    TINGLEY, JV
    BONHAM, HF
    ECONOMIC GEOLOGY AND THE BULLETIN OF THE SOCIETY OF ECONOMIC GEOLOGISTS, 1994, 89 (02): : 401 - 407
  • [5] HYDRATION AND DEHYDRATION OF ZEOLITIC TUFF FROM YUCCA MOUNTAIN, NEVADA
    KRANZ, RL
    BISH, DL
    BLACIC, JD
    GEOPHYSICAL RESEARCH LETTERS, 1989, 16 (10) : 1113 - 1116
  • [6] Factors limiting microbial activity in volcanic tuff at Yucca Mountain
    Kieft, TL
    Kovacik, WP
    Taylor, J
    HIGH LEVEL RADIOACTIVE WASTE MANAGEMENT, 1996 ., 1996, : 36 - 38
  • [7] Geological Disposal of Nuclear Waste in Tuff: Yucca Mountain (USA)
    Swift, Peter N.
    Bonano, Evaristo J.
    ELEMENTS, 2016, 12 (04) : 263 - 268
  • [8] Creep and static fatigue of welded tuff from Yucca Mountain, Nevada
    Martin, R.J.
    Noel, J.S.
    Boyd, P.J.
    Price, R.H.
    International Journal of Rock Mechanics and Mining Sciences, 1997, 34 (3-4): : 1 - 190
  • [9] PALEOGEOTHERMAL AND PALEOHYDROLOGIC CONDITIONS IN SILICIC TUFF FROM YUCCA MOUNTAIN, NEVADA
    BISH, DL
    ARONSON, JL
    CLAYS AND CLAY MINERALS, 1993, 41 (02) : 148 - 161
  • [10] Feldspar dissolution rates in the Topopah Spring Tuff, Yucca Mountain, Nevada
    Bryan, Charles R.
    Helean, Katheryn B.
    Marshall, Brian D.
    Brady, Patrick V.
    APPLIED GEOCHEMISTRY, 2009, 24 (11) : 2133 - 2143