570 METH^MOGLOBIN. [BOOK n. 



Though not crystallizable itself, huiematin forms with hydro- 

 chloric acid a compound, occurring in minute rhombic crystals, 

 known as hcemin crystals. 



When blood is left until it decomposes, the haemoglobin is very 

 apt to become changed into a peculiar body known as nwthfBnw- 

 fjlobin, in the spectrum of which a very conspicuous band is seen 

 in the red between C and D (see Fig. 76, 4). The same change 

 may be brought about by the action of weak acids, such as 

 carbonic acid, by ozone, and by other agents such as nitrites and 

 potassium permanganate. When a stream of carbonic acid is 

 driven through blood or through a solution of haemoglobin the 

 band in the red characteristic of methaemoglobin soon makes 

 its appearance. Metha-moglobin differs but little it' at all in 

 elementary composition from haemoglobin ; it is maintained that 

 it contains the same quantity of oxygen as oxy-ha^moglobrn but 

 in a more stable condition, more intimately associated with the 

 molecule. 



In conclusion, the condition of oxygen in the blood is as 

 follows. Of the whole quantity of oxygen in the blood, only a 

 minute fraction is simply absorbed ( .r dissolved according to the 

 law of pressures (the Henry- Dalton law). The great mass is in a 

 stare of combination with the luemoglobin, the connection being of 

 such a kind that while the haemoglobin readily combines with the 

 "\ygeii of the air to which it is exposed, dissociation readily occurs 

 at low pressures, or in the presence of indifferent ^ases, or by the 

 action of substances having a greater affinity for oxygen than has 

 haemoglobin itself. The difference between venous and arterial 

 blood, as far as oxygen is concerned, is that while in arterial 

 blood the haemoglobin holds nearly its full complement of oxygen 

 and may be spoken of a- nearly wholly oxyruemoglobin, in venous 

 blood the haemoglobin is to a large but variable extent, reduced ; 

 and the characteristic colours of venous and arterial blood are in 

 the main due to the fact that the colour of reduced haemoglobin 

 is purple, while that of oxyhgemoglobin is scarlet. 



The relations of the Carbonic Acid in the Blood. 



352. The presence of carbonic acid in the blood appears to 

 be determined by conditions more complex in their nature and at 

 present not so well understood as those which determine the 

 presence of oxygen. The carbonic acid is not simply dissolved in 

 the blood ; its absorption by blood does not follow the law of 

 pressures. 7 It exists in association with some substance or sub- 

 stances in the blood, and its escape from the blood is a process of 

 dissociation. 'We cannot however speak of it as being associated, 

 to the same extent as is the oxygen, with the haemoglobin of the 

 red corpuscles. So far from the red corpuscles containing the 

 great mass of the carbonic acid, the quantity of this gas which is 



