24: 



MINERAL WATERS. 



Fresenius, R. Analyse dor fiinf Eisen-Quellen in Bad Neudorf in 

 Bohmcn. [5 Iron-Springs, Neudorf, Bohemia.] 8vo. Wiesbaden. 



. Anal5'se der Mineral-Quelle bei Birrcsborn in der Eifel. 



[Mineral Spring in tlie Eifel,] 8vo. Wiesbaden. 



Analyse der warmen Quelle zu Assmannshausen. [Thermal 



Spring at Assmannshausen.] 8vo. Wiesbaden. 



Chemisehe Analyse der Mineral-Quelle bei Biskirchen im 



Lahnthale. [Mineral Spring in the LahnYalley.] 8vo. Wiesbaden. 



Godefroy, Dr. Rich. Das Fischauer Badewasser. [The Fischau 

 Spa.] Zeitsch. alJgem. aster r. Apothelc.-Ver. Bd. xiv. no. 16. 



Heinrichs, Prof. On Waters of deep-lying rocks of Iowa, resembling 

 the waters of the sea. Nature, vol. xv. p. 303. 



Hirschfeld, Dr., and Dr. Pichler. Die Biider, Quellon und Curorto 

 Europa's. [The Baths, Springs, and Health-llesorts of Europe.] 

 2 vols. Stuttgart, 1875-1876. 



Jervis, "William. Guida alle aequo minerali d'ltalia, Provincio 

 meridional]. [Guide to the Mineral Waters of S. Italy.] Pp. 320 ; 

 14 plates. 8vo. Turin. 



Loebisch, Dr. W. P., and L. Sipbcz. Analyse des Wassers vora 

 " !Mare Morto " auf der Insel Lacroma. [Analysis of Water of the 

 " Dead Sea " on the I. of Lacroma.] Min. Mitth. Heft iii. pp. 

 171-174. 

 Sp. gr. of the water at 17°'6 C. = 1*0245. Results of analysis tabu- 

 lated as (in 10,000 parts of water) NaCl 222-7060, MgCl^ 42-4634, 

 CaCl., 10-9663, MgBr, 0-9650, MgCOg 3-1835, K^SO^ 7-8340, and 

 Na/0, 29-3204. F. W. R. 



Ludwlg, E. Chemisehe Anal5^se der Darkauer jodhaltigen Salzsoolc. 

 [Analysis of the Iodine-saline Spring of Darkau.] Min. Mitth. 

 Heft ii. pp. 119-132. 



The mineral water at Darkau, in Austrian Silesia, had a temp, of 

 11°- 75 C, that of the air being 6° C. Its sp. gr. is 1-01865. Details of 

 analysis are given. It contains -002256 p. e. of iodine, and -01097 of 

 bromine. Gas extracted from the water contained 25-64 p. c. of CO^, 

 51-74 of CHj, and 22-62 of N. Free gas is also disengaged from tho 

 spring ; and of this ananalys is is given. The same constituents are 

 present as in the dissolved gas. The water is notable for its excep- 

 tional richness in l)romine. F. W. R. 



