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Development of portable, visible to infra-red spectrometer to measure geophysical and geochemical properties of rocks

Development of portable, visible to infra-red spectrometer to measure geophysical and geochemical properties of rocks
开发便携式可见红外光谱仪来测量岩石的地球物理和地球化学性质
批准号:
05504002
负责人:
TADA Ryuji
金额:
$23.1万
依托单位:
依托单位国家:
日本
项目类别:
Grant-in-Aid for Developmental Scientific Research (A)
财政年份:
1993
资助国家:
日本
项目状态:
已结题
起止时间:
1993 至 1995

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中文摘要
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英文摘要
In this research, we developed portable, visible to near infra-red spectrometer (Geosensor) which is 228x308x172 mm in size, 8 kg in weight, possessing its own light source, and capable of measuring reflection intensity over the wide wave length ranging from 400 nm to 2500 nm within 8 seconds with the resolution of less than 6 nm. The first year was spent almost entirely to construct the instrument. Tests both in the laboratory and in the field (out-door) were repeated to evaluate its precision, reproducibility, and other specification and to improve its usability to meet our requirements. Although the reproducibility within the wave range of 400 to 700 nm and 2400 to 2500 nm was not good enough, its resolution and reproducibility was both acceptable in the wave range of 700 to 2400 nm. From the later half of the second year to the third year, we moved to the next step to explore its applicability in the field geoscience. First, we measured reflective spectra for various rock types, an … More d found that Geosensor is capable of identifying broad absorb peaks situated at 550 nm and 900 nm attributable to Fe^<3+>, broad absorb peak situated at 1100 nm attributable to Fe^<2+>, relatively sharp absorb peaks at 1400 and 1900 nm attributable to water, sharp peaks situated at 1400,2200, and 2450 nm attributable to -OH,and sharp peak situated at 2350 nm attributable to CO3^<2->. Next we experimentally examined the controlling factors which influence the intensity of the absorb peak (absorbance) of water. The result suggests that the absorbance is mainly controlled by such factors as water content, grain size, and contents of opaque grains. The result further suggests that if we restrict the rock type as fine grained sediments with relatively similar water contents, we can estimate contents of opaque grains based on quick measurements by Geosensor. We applied this method to actual sediment core samples recovered from Japan Sea to estimate organic carbon and pyrite contents and obtained satisfactory result. Less
期刊论文(30)
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会议论文
入野智久: "Eauripik Rise KH92-1,56PCコアから見た過去20万年間の西赤道太平洋深海堆積物中の砕屑物組成変化" 月刊地球. (in press). (1994)
Tomohisa Irino:“从 Eaulipik Rise KH92-1,56PC 核心观察到的过去 20 万年中赤道西太平洋深海沉积物中碎屑成分的变化”,《地球月刊》(1994 年)。
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黒木紀子: "岩石の酸化反応のその場測定" 月刊地球. (in press). (1995)
Noriko Kuroki:“岩石氧化反应的原位测量”,地球月刊(1995 年)。
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通讯作者:
黒木紀子: "岩石の酸化反応のその場測定" (in press). (1996)
Noriko Kuroki:“岩石氧化反应的原位测量”(正在出版)(1996 年)。
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29
    Changes in hydrological cycle in East Asia during the Holocene and their implication for Global Monsoon
    • 批准号:
      23221002
    • 项目类别:
      Grant-in-Aid for Scientific Research (S)
    • 资助金额:
      $138.36万
    • 财政年份:
      2011
    • 负责人:
      TADA Ryuji
    • 依托单位:
    Paleoceanography for future prediction : a possibility of climate mode jump with global warming
    • 批准号:
      18101001
    • 项目类别:
      Grant-in-Aid for Scientific Research (S)
    • 资助金额:
      $69.89万
    • 财政年份:
      2006
    • 负责人:
      TADA Ryuji
    • 依托单位:
    High-resolution reconstruction of the paleoceanographic changes in the Japan Sea in response to the rapid changes in Asian monsoon
    • 批准号:
      15310008
    • 项目类别:
      Grant-in-Aid for Scientific Research (B)
    • 资助金额:
      $7.3万
    • 财政年份:
      2003
    • 负责人:
      TADA Ryuji
    • 依托单位:
    Testing the presence of the climate mode warmer than present based on the paleoenvironmental analysis
    • 批准号:
      12308026
    • 项目类别:
      Grant-in-Aid for Scientific Research (A)
    • 资助金额:
      $16.28万
    • 财政年份:
      2000
    • 负责人:
      TADA Ryuji
    • 依托单位:
    海外基金