UC-NRLF ^3 GREGORY . . ON . . P£RTILtI2HRS« http://www.archive.org/details/fertilizerswhereOOgregrich m FERTILIZERS. WHERE THE MATERIALS COME FROM. WHERE TO GET THEM IN THE CHEAPEST FORM, HOW TO COMPOUND FORMULAS, ETC., ETC. BY J. J. H. GREGORY, A.M., AUTHOB OF WORKS ON CABBAGK -RAISING, ONION-RAISING, SQUASH-RAISIHe, STC Copyb:ght, 18«3, Bt 0. J. H. GREGORir. »»•.<• PREFACE, This treatise is by a farmer for farmers. Using forty or fifty tons of commercial fertilizers on my own crops annually, I have been compelled to " book myself up," as the phrase is, — to learn the cheapest market in which to buy the elements, the best way to combine these, and the wisest way to apply them to the different crops of the farm. This treatise is the result of the study of various works on agricultural chemistry, especially the excellent reports that have been sent out from our agricultural stations by Professors. Johnson and Atwater, Goessmann, Dabney, Caldwell, and others, to whom our sense of indebtedness will be measured by the growth of our intelligence. This study, combined with personal observation and experience, makes up my little book. My treatise is not a work on barn manure : it is confined, for the most part, to fertilizers. It can perform no miracles : to ask that it shall show every one the road to success in the profitable raising of his crops would be as reasonable as was the search of the alchemist of old for the wonderful alembic that was to transmute every thing to gold. The whole matter of soil 240791 •" IV PREFACE. action and plant-growth is wonderfully complex ; and so far from the old axiom being true, that any man can be a farmer, we find that farming, in the problems it presents for solution, is a calling that challenges the best ability and the best culture to be found among men. To give a history of the three principal elements which enter into the composition of fertilizers, to discuss their relations to plant-growth in the various forms in which they exist, to tell in what form and where they may be obtained at the lowest rates, to tell how they may be combined and applied' in the wisest way, brother farmers, is the object of this treatise. Should it prove desirable to enlarge the subject, I may take up barn and various other manures in another work. To those who desire to study the subject of. plants and plant-growth more extensively, I would recommend such excellent works as " How Crops Grow " and " How Crops Feed," by Professor Johnson ; " Botanical Text-Book," by Professor Grey ; and " Harris on Manures." CONTENTS, PAOB Introduction 1 Difference between Barn Manure and Commercial Fertilizers ... 6 What is Barnyard Manure ? 8 Humus 12 Are Fertilizers but Stimulants ? 13 Potash 16 Wood Ashes 23 Coal Ashes 29 Cotton-Seed Hulls 29 The Uses of Potash in Agriculture What is Nitrogen ? Where Nitrogen or Ammonia comes from 35 How to Handle Fish- Waste, and the Best Way to Feed it to the Crops, 40 Other Sources for Nitrogen 44 Phosphoric Acid 54 Bones, and where they come from 57 Making our own Superphosphate 58 Reduction of Unground Bone 64 The Theories of Fertilizing 68 Testing our Soils 72 A Faith that is Dangerous ; Buying Cheap Fertilizers ..... 74 Making our own Fertilizers 77 The Manufacturers of Fertilizers 78 Leather-Waste 79 Some Facts and Suggestions 81 Fertilizing Ingredients in Raw Materials and Chemicals 84 Commercial and Agricultural Values of Fertilizers 86 Where to Obtain our Fertilizing Material at the Lowest Cost ... 86 Formulas, and how to Compound them 90 Formulas for Various Crops 91 How to Compound our own Formulas 94 Some Formulas as Compounded 96 Condensation of Special and other Formulas 98 How to Mix the Ingredients that enter into a Formula 101 Applying Fertilizers 102 The System of Manuring with Unleached Wood Ashes 103 Fertilizers Excellent for Various Crops, and Suggestions .... 105 Composts 108 American Analyses of Composition of Fertilizing Materials . . Ill, 112 Estimates of Cost of Plant-Food in Crops 114 A Plea for Mercy 115 FERTILIZEK8. INTRODUCTION. Chemists tell us that water, and this air around us, that we can neither see nor grasp, and which in all our every- day calculations of space we take no account of, make up from eighty-eight to ninety-nine per cent of our crops, our trees, or any form of vegetable growth. Practically, we know this is so ; for we can bring out in a bushel-basket all the ashes made from a load of wood that it might take a couple of yoke of oxen to draw in. A wood cord is about one hundred bushels ; in the ashes which contain the min- erals that entered into the make-up of that wood, we get not more than two per cent of this. The great remainder, after yielding that heat which the sun has fed to it for, it may be, a hundred years, in the form of vapor and gases hurries up the chimney, to return to mother-air, from whence they came. Plant-life builds up the mighty tree, borrowing almost nothing from the soil. It is the weight of the air and the water present in its structure that our oxen strain under when hauling to mill the trunk of some huge veteran of the forest. All that it has taken from the soil to make up its huge bulk the driver might carry in a bag on his shoulder, and then have to go some distance to get an appetite for breakfast. In brief, to express it in 1 ^ FERTILIZERS. . . . • < o ( a 'familiar- way, i&^ii does but little more than help plants. ; ^tand .upright ; while water and air, obeying chemical ' laws, build up their structure. And what is soil? It is the result of the destruction of the rocks mingled with vegetable waste ; it is the turning of all life, organic and inorganic, into its original elements ; it is the great grave- yard of creation ; it is the great mine of the world, out from which come the food of all animal and vegetable life, the wherewithal they shall be clothed, the means of shelter and protection from heat, cold, and wet ; it is Mother Earth, from whom all organized life springs, and to whom, after completing its little round, all matter that enters therein returns, to repose a while within her bosom, there to rest and refresh itself before entering into new forms, and running another course of vitality. " The earth is my mother," said Red Jacket, the Indian orator, at the Great Council, declining a chair offered him : " I will rest upon her bosom." Yes, she is the material mother of all organized life; and, when their course is ended, all her children go home to her. The giant of the forest may span his thousand years of time, and, towering upward a hundred feet above his fellows, may seem to despise his humble origin ; but his mother is patiently waiting for him : and, hoary with years, worn and weary, seeking rest, he bows his lofty head, falls upon her breast, and receives her final embrace. Man himself, standing at the head of all organized life, in sleep, imago mortis, reclines by instinct on her bosom ; and, when comes the final hour, his material self by loving hands is gently lowered into her yearning care, " dust unto dust." If any man could really believe that this is the final end, he would that instant die of horror, or become insane. The cheer that every good deed leaves in our hearts is full of the instinct of immortality. FERTILIZERS. 3 If we give the bushel of ashes into the hands of the chemist, to tell us what it is made of, he will return us silicon, potassium, calcium, phosphorus, sodium, alumin^ ium, sulphur, iron, chlorine, magnesium. These are the elements that all plants take from the soil. The soil itself obtained them originally from the ledges of solid rock, which through eons of years have been slowly disinte- grating and decomposing. Geology tells us, that, by the action of the drift waves of ancient eras, mountains of water six thousand feet or more in height swept from the. north, breaking down, filling up, and smoothing off, the ragged, craggy surface of the ancient lava-covered earth ; by later glacial action, and that of water and frost, which extend into the human period, the rocks have been ground up, and scattered over a large portion of the surface of our planet in gravelly hills and plains, covered more or less by vegetable matter, through which protrude, in places* the rocky ribs of the ancient earth. This soil is but a sprinkling on the surface of our globe. At a depth of but a few hundred feet, at the utmost, on any spot of its mil- lions of miles of surface, we would strike rock, solid to the great lava centres. The principal ledges from which have come originally the mineral matter of the soil, are of the granite class. These yield the minerals felspar, mica, hornblende, and quartz ; and they, the silicon, potash, iron, alumina, soda, lime, and manganese. The sedimentary rocks, of which the various slates are a type, have the particles in a finer forin than they exist in the parent primary rocks ; and hence the soils formed from these, such as the clays, have the mineral constituents in a finer condition. But the finest subdivis- ion of all, in which the mineral matter of the soil exists, is that supplied by dead plant and animal life, into whose structure the minerals entered in so fine a state as to be held in solution by water.