K. KANESHIMA (1969) reported on chemical analyses of waters on the SENKAKU RETTO. The present authors made calculations based on his data and discussed behaviors of Na^+, K^+, Ca^2+, Mg^, H^+, C1^-, SO_4^, PO_4^, and HCO_3^-, in hydrosphere, atomosphere, and Iithosphere. As a result, they obtained new informations about water's history on the SENKAKU RETTO which may be summarized as follows: (1) All seven samples were supporsed to be made of land waters being mixed with sea water by some means on the each islands. The mixing rate of sea water for 1 liter of land waters is 1/140 liter for sample No. 1, 1/100 liter for No.2, 1/100 liter for No.3, 1/130 liter for No.4, 1/70 liter for NO.5, 1/80 liter for No.6 and 1/60 liter for No.7. (2) Altho...
The chemical and physical characteristics of the thermal and ground waters in Sekigane Hot Springs w...
We have carried out chemical analyses on springs and underground waters collected from 31 localities...
This paper traces the origin of anions of groundwaters in Mushigame landslide area. The groundwaters...
The waters on both Minami and Kita Daito Jima have been collected, to discuss the geochemical nature...
From March 22 to March 29,1972. the University of the Ryukyus has conducted a scientific survey of Y...
Chemical and physical studies on 304 water samples collected from Iriomote-Island, Ishigaki-Island, ...
What are the natural states in OKINAWA HONTŌ? A part of the authors' purposes is to get knowledge ab...
The ground waters on both GIJI and KIAN have been collected, to discuss the geochemical nature of wa...
Spring waters (54 samples) were collected from the landslide area and stable area in Yamakoshi villa...
We determined the chemical compositions and tritium concentration of precipitations sampled from the...
In OKINAWA HONTO, the Cl^- concentrations of river and spring waters are 20-50 ppm. What mechanisms ...
The author determined some chemical components of brine waters occurred from gas field in Okinawa so...
Geochemical studies were conducted on natural waters in TAKANA and KOMI regions and the main four ri...
Ground waters are sampled from observation wells bored to measure ground water levels in Nagaoka and...
Three samples of mineral spring water were collected from Yashio Mineral spring, Gumma Prefecture, a...
The chemical and physical characteristics of the thermal and ground waters in Sekigane Hot Springs w...
We have carried out chemical analyses on springs and underground waters collected from 31 localities...
This paper traces the origin of anions of groundwaters in Mushigame landslide area. The groundwaters...
The waters on both Minami and Kita Daito Jima have been collected, to discuss the geochemical nature...
From March 22 to March 29,1972. the University of the Ryukyus has conducted a scientific survey of Y...
Chemical and physical studies on 304 water samples collected from Iriomote-Island, Ishigaki-Island, ...
What are the natural states in OKINAWA HONTŌ? A part of the authors' purposes is to get knowledge ab...
The ground waters on both GIJI and KIAN have been collected, to discuss the geochemical nature of wa...
Spring waters (54 samples) were collected from the landslide area and stable area in Yamakoshi villa...
We determined the chemical compositions and tritium concentration of precipitations sampled from the...
In OKINAWA HONTO, the Cl^- concentrations of river and spring waters are 20-50 ppm. What mechanisms ...
The author determined some chemical components of brine waters occurred from gas field in Okinawa so...
Geochemical studies were conducted on natural waters in TAKANA and KOMI regions and the main four ri...
Ground waters are sampled from observation wells bored to measure ground water levels in Nagaoka and...
Three samples of mineral spring water were collected from Yashio Mineral spring, Gumma Prefecture, a...
The chemical and physical characteristics of the thermal and ground waters in Sekigane Hot Springs w...
We have carried out chemical analyses on springs and underground waters collected from 31 localities...
This paper traces the origin of anions of groundwaters in Mushigame landslide area. The groundwaters...