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ents of plants within about the above named distance from the surface of the soil. If such were not the case, the fertility of the earth must soon be destroyed, as all of those elements which the soil must supply to growing plants would be carried down out of the reach of roots, and leave the world a barren waste, its surface having lost its elements of fertility, while the downward filtration of these would render the water of wells unfit for our use. Now, however, they are all retained near the surface of the soil, and the water issues from springs comparatively pure. EVAPORATION removes from manure-- Carbon, in the form of carbonic acid. Hydrogen and oxygen, in the form of water. Nitrogen, in the form of ammonia. LEACHING removes from manure-- The soluble and most valuable parts of the ash in solution in water, besides carrying away some of the named above forms of organic matter. FOOTNOTES: [X] It should be recollected that every bent straw may act as a syphon, and occasion much loss of liquid manure. CHAPTER IV. ABSORBENTS. [What substances are called absorbents? What is the most important of these? What substances are called charcoal in agriculture? How is vegetable matter rendered useful as charcoal?] Before considering farther the subject of animal excrement, it is necessary to examine a class of manures known as _absorbents_. These comprise all matters which have the power of absorbing, or soaking up, as it were, the gases which arise from the evaporation of solid and liquid manures, and retaining them until required by plants. The most important of these is undoubtedly _carbon_ or charcoal. CHARCOAL. _Charcoal_, in an agricultural sense, means all forms of carbon, whether as peat, muck, charcoal dust from the spark-catchers of locomotives, charcoal hearths, river and swamp deposits, leaf mould, decomposed spent tanbark or sawdust, etc. In short, if any vegetable matter is decomposed with the partial exclusion of air (so that there shall not be oxygen enough supplied to unite with all of the carbon), a portion of its carbon remains in the exact condition to serve the purposes of charcoal. [What is the first-named effect of charcoal? The second? Third? Fourth? Explain the first action.] The offices performed in the soil by carbonaceous matter were fully explained in a former section (p. 79, Sect. 2), and we will now examine mere
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