Migration of chemical elements through phases of the atmosphere, hydrosphere and lithosphere in the Juneau Glacier area. I
The Juneau Icefield area is thought to be one of the best locations for the geochemical study on the migration of chemical elements through the hydrosphere. In this report, the migration of chemical species, Na+, Ca2+, Mg2+, Cl-, SO42-, HCO3-, molybdate-reactive silica and borate-boron, is discussed...
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| Published in | GEOCHEMICAL JOURNAL Vol. 3; no. 2-3; pp. 99 - 115 |
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| Main Authors | , , , , , , , |
| Format | Journal Article |
| Language | English |
| Published |
GEOCHEMICAL SOCIETY OF JAPAN
1969
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| Abstract | The Juneau Icefield area is thought to be one of the best locations for the geochemical study on the migration of chemical elements through the hydrosphere. In this report, the migration of chemical species, Na+, Ca2+, Mg2+, Cl-, SO42-, HCO3-, molybdate-reactive silica and borate-boron, is discussed. The following facts were pointed out: (1) the major chemical species other than calcium and bicarbonate ions in saline water of the area mainly come from sea water, (2) calcium and bicarbonate ions in large amount are supplied to saline water by dissolution of carbonate material contained in muddy sediments which are formed by glacial erosion, (3) removal of soluble silica must be assumed when muddy fresh water from glaciers mixes with sea water to form saline water, (4) the silica content of suspended material decreases with increasing salt content of saline water, and (5) the ratio of borate-boron concentration to chloride concentration is higher in interstitial water than in saline water. |
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| AbstractList | The Juneau Icefield area is thought to be one of the best locations for the geochemical study on the migration of chemical elements through the hydrosphere. In this report, the migration of chemical species, Na+, Ca2+, Mg2+, Cl-, SO42-, HCO3-, molybdate-reactive silica and borate-boron, is discussed. The following facts were pointed out: (1) the major chemical species other than calcium and bicarbonate ions in saline water of the area mainly come from sea water, (2) calcium and bicarbonate ions in large amount are supplied to saline water by dissolution of carbonate material contained in muddy sediments which are formed by glacial erosion, (3) removal of soluble silica must be assumed when muddy fresh water from glaciers mixes with sea water to form saline water, (4) the silica content of suspended material decreases with increasing salt content of saline water, and (5) the ratio of borate-boron concentration to chloride concentration is higher in interstitial water than in saline water. |
| Author | Yoshioka, Ryuma Hood, Donald W. Kitano, Yasushi Kato, Kikuo Kanamori, Satoru Kanamori, Nobuko Knowles, Leonard I. Kunze, George W. |
| Author_xml | – sequence: 1 fullname: Kitano, Yasushi organization: Water Research Laboratory, Faculty of Science, Nagoya University – sequence: 2 fullname: Kanamori, Satoru organization: Water Research Laboratory, Faculty of Science, Nagoya University – sequence: 3 fullname: Kato, Kikuo organization: Water Research Laboratory, Faculty of Science, Nagoya University – sequence: 4 fullname: Kanamori, Nobuko organization: Water Research Laboratory, Faculty of Science, Nagoya University – sequence: 5 fullname: Yoshioka, Ryuma organization: Water Research Laboratory, Faculty of Science, Nagoya University – sequence: 6 fullname: Knowles, Leonard I. organization: Douglas Marine Station, University of Alaska – sequence: 7 fullname: Kunze, George W. organization: Department of Soil and Crop Sciences, Texas A and M University – sequence: 8 fullname: Hood, Donald W. organization: Institute of Marine Science, University of Alaska |
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| References | KUNZE, G. W., KNOWLES, L. I. and KITANO, Y. (1968) The distribution and mineralogy of clay minerals in the Taku Estuary of southeast Alaska. Marine Geol. 6, 439-448. UTSUMI, S. (1952) A new spectrophotometric determination of small amounts of chloride ions with mercury thiocyanate and iron ammonium sulfate. J. Chem. Soc. Japan (Nippon Kagaku Zasshi) 73, 835-841. (in Japanese) GREENHALGH, R. and RILEY, J. P. (1962) The development of a producible spectrophotometric curcumin method for determining boron, and its application to sea water. Analyst 87, 970-976. KANAMORI, N. and KITANO, Y. (1966) Spectrophotometric determination of small amounts of magnesium in natural waters and carbonate sediments. J. Earth Sciences, Nagoya Univ. 14, 1-9. SUGAWARA, K. (1964c) Migration of elements through phases of atmosphere and hydrosphere. III. ibid. 6, 359-364. JANSEN, J. J. and KITANO, Y. (1963) The resistance of recent marine carbonate sediments to solution. J. Ocean. Soc. Japan 18, 42-53. KANAMORI, S. and SUGAWARA, K. (1965b) Geochemical study of arsenic in natural waters. II. Arsenic in river water. ibid. 13, 36-45. KITANO, Y., KATO, K., KANAMORI, S., KANAMORI, N. and YOSHIOKA, R. (1967) Rockslides resulting from the geochemical weathering of parent materials. Annuals, Disaster Prevention Res. Inst., Kyoto Univ. 10A, 557-587. SUGAWARA, K. (1964b) Migration of elements through phases of atmosphere and hydrosphere. II. ibid. 6, 317-321. IWASAKI, I., UTSUMI, S., HAGINO, T., TARUTANI, T. and OZAWA, T. (1958) A new spectro-photometric determination of small amount of sulfate ions with barium chromate and diphenylcarbazide. J. Chem. Soc. Japan (Nippon Kagaku Zasshi) 79, 32-50. (in Japanese) KATO, K. and KITANO, Y. (1966) Salt error in colorimetric determination of the molybdate-reactive silica in sea water. ibid. 14, 151-158. KANAMORI, S. and SUGAWARA, K. (1965a) Geochemical study of arsenic in natural waters. I. Arsenic in rain and snow. ibid. 13, 23-35. KNOWLES, L. I., KUNZE, G. W. and KITANO, Y. (in preparation) FORBES, R. B. (1959) The geology and petrology of the Juneau Ice Field area, southeastern Alaska. PhD Thesis, Univ. Washington 1-259. SUGAWARA, K. (1964a) Migration of elements through phases of atmosphere and hydrosphere. I. J. Water and Waste 6, 227-230. EK, C. (1964) Note sur les eaux de fonte des glaciers de la Haute Maurienne. Leur action sur les carbonates. Revue Belge de Geographic 88, 127-156. |
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