254 



SCIENCE OF GARDENING. 



Part II. 



Chap. IV. 



Of the Agency of the Atmospliere in Vegetation. 



1215. The aerial medium ivhich efivelopes the earth may be studied chemically and phy- 

 sically ; the first study respects the elements of which the atmosphere is composed ; and 

 the second theii- action in a state of combination, and as influenced by various causes, 

 or those phenomena wliich constitute the weather. 



Sect. I. Of the Elements of the Atmosphere. 



1216. Water, carbonic acid gas, oxygen, and azote, are tlie principal substances composing 

 the atmosphei'e ; but more minute enquiries respecting their natm'e and agencies are 

 necessary to afford coiTCCt views of its uses in vegetation. 



1217. That loater exists in the atmosphere is easily proved. If some of the salt, called 

 muriate of lime, that has been just heated red, be exposed to the air, even in the di iest 

 and coldest weather, it will increase in weight, and become moist ; and in a certain time 

 will be converted into a fluid. If put into a retort and heated, it will jdeld pure water ; 

 will gradually recover its pristine state ; and, if heated red, its former weight : so that it 

 is evident that the water united to it was derived from the air. And that it existed in 

 the air in an invisible and elastic form, is proved by the circumstance, that if a given 

 quantity of air be exposed to the salt, its volume and weight will diminish, provided th« 

 experiment be correctly made. 



1218. The quantity of water which exists in air, as vapor, varies vdih the temperature. In 

 proportion as the weather is hotter, tlie quantity is greater. At 50° of Fahj-enheit, 

 air contains about one 50th of its volume of vapor ; and as the specific gravity of vapor 

 is to that of air nearly as 10 to 15 ; this is about one 75th of its weight. At 100°, sup- 

 posing that there is a free communication with, water, it contains about one 14th part 

 in volume, or one 21st in weight. It is the condensation of vapor by diminution of the 

 temperature of the atmosphere, which is probably the principal cause of the formation of 

 clouds, and of the deposition of dew, mist, snow, or hail. 



1219. The power of differetit substances to absorb aqueous vapor from the atmosphere by 

 cohesive attraction has been already refened to. (1058.) The leaves of li\-ing plants ap- 

 pear to act upon this vapor in its elastic form, and to absorb it. Some vegetables 

 increase in weight from tliis cause, when suspended in the atmosphere and unconnected 

 with the soil; such are the house-leek, and different species of the aloe. In very 

 intense heats, and when the soil is dry, the life of plants seems to be preserved by the 

 absorbent power of their leaves ; and it is a beautiful circumstance in the economy 

 of nature, that aqueous vapor is most abundant in the atmosphere when it is most 

 needed for the purposes of life j and that when other sources of its supply are cut off, 

 this is most copious. 



1220. The existence of carbonic acid gas in the atmosphere is proved by the following 

 process : if a solution of lime and water be exposed to the air, a pellicle will speedily 

 form upon it, and a solid matter will gradually fall to the bottom of the water, and in a 

 certain time the water will become tasteless ; this is owing to the combination of the lime 

 which was dissolved in the water with carbonic acid gas, which existed in the atmosphere, 

 as may be proved by collecting the film and the solid matter, and igniting them strongly 

 in a little tube of platina or iron ; they will give out carbonic acid gas, and will become 

 quick-lime, which, added to the same water, will again bring it to the state of lime- 

 water. 



1221. The quantity of carbonic acid gas in the atjnosphere is very small. It is not easy 

 to determine it with precision, and it must differ in different situations ; but where tliere 

 is a free circulation of air, it is probably never more than one 500th, nor less than one 800th 

 of the volume of air. Carbonic acid gas is nearly one thu-d heavier than the other elastic 

 parts of the atmosphere in their mixed state ; hence at first view it tnight be supposed 

 that it would be most abundant in the lower regions of the atmosphere ; but unless it has 

 been immediately produced at the surface of the earth in some chemical process, this does 

 not seem to be the case ; elastic fluids of diflPerent specific gravities have a tendency to 

 equable mixture by a species of attraction, and the different parts of the atmosphere are 

 constantly agitated and blended together by winds or other causes. De Saussure found 

 lime-water precipitated on Mount Blanc, the highest point of land in Europe ; and 

 carbonic acid gas has been always foimd, apparently in due proportion, in the air brought 

 down from great heights in the atmosphere by aerostatic adventurers. 



1222. The principal consumption of the carbonic add in the atmosphere seems to be in 

 affording nourishment to plants ; and some of them appear to be sup|)lied with carbon 

 chiefly from this source. 



1223. The formation of carbonic acid gas takes place during fermentation,* combustion, 

 putrefaction, respiration, and a number of operations taking place upon the surface of the 



