The distribution of air ion at 20 hot springs in Japan was surveyed in 1961, and results obtained were as follows:
1) Each number of air ion-density at twenty hot springs is as follows: Dogo spa (2, 208/cc), Onne-yu (1, 293), Beppu (1, 257), Echigo-yuzawa (1, 197), Misasa (1, 187), Karurusu (1, 179), Ito (1, 094), Naruko (1, 019), Shiobara (947), Arima (931), Jozankei (895), Nasu (848), Kawayu (827), Tokachigawa (781), Toya (761), Yunokawa (720), Kusatsu (719), Tsuchiyu (610), Noboribetsu (563), Akan (469).
2) Each value of radium emanation is as follows: Misasa spa (157, 0ME), Yunokawa Dogo, Tsuchiyu, Karurusu, Tokachigawa, Jozankei, Ito, Onneyu, Noboribetsu, Shiobara, Akan, Echigoyuzawa, Beppu, Toya, Arima, Kawayu, and Kusatsu.
3) The more acid hot spring water is, the higher air ion-density is observed.
4) The more acid hot soring water is, the more the ratio of n
+/n
- is observed.
5) The more alkaline hot spring water is, the higher the value of radium emanation is found.
6) The higher the value of radium emanation is, the higher air ion-density is found.
7) The lower temperature of spring is, the higher air ion-density is found.
8) In simple thermals, common salt springs, and radioactive springs, high air iondensity is observed.
9) The higher acidity of the rock is, the higher air ion-density and the value of radium emanation are days.
10) Air ion-density in hot spring zone tends to increase most frequently in rainy, and next in cloudy, and rarely in fine days.
11) The ratio of n
+/n
- is the smallest in rainy and the largest in cloudy weather.
12) Air ion-density is high in the case of north westerlies, and conversely, it is low in the case of south-easterlies
13) Density of n
- increases in the case of north-easterlies, conversely density of n
+ increses in south-easterlies.
14) Effects of air ion on human body are as follows: n
- acts parasympaticotonically and n
+ acts sympaticotonically.
View full abstract