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VOL. LXI PUBLIC LIBRARY INDIANAPOLIS, JULY 28, 1906. NO. 30 SOILS AND QRUN CROPS. With Some Soils Everything Depends on Oiven Rain Pall. Conserving Moisture in Dry Seasons on Clay Subsoils. Moisture in Production. The following . hows the proportion of water to dry matter, grain aiid straw, in producing the crops named. 1. W heat 400 lbs. water to 1 lb of dry matter. Oats 500 lbs. water to lib. of dry matter. Corn 300 lbs water to 1 lb. of dry matter. Timothy and clover require I he same proportion of water to dry matter that wheat does to produce them. 2. 3. Scientific investigations have settled many primary considerations in crop trowing, and especially as regards grain crops. It is well to keep these well-settled facts in mind, as they relate to seasons, and soils and rainfall. When the season brings the normal rainfall and it ! is well distributed through the growing months of the cropping year, there is little or no uncertainty of crop-growing results on any of our soils. But when- the rainfall is below 28 to 30 inches a year, and not well distributed through the growing season, there is little help for the growing crops on the soils having sand and gravel beneath them, for upon such the moisture quickly leaches away and the plant is left helpless. With clay subsoils in such seasons it is different. Deep plowing leaves below it a reservoir which holds the moisture to be used by capillary action at the roots of the growing plants. The first mentioned soil formation, with porous conditions below, are found in several parts of Indiana, including a considerable area of Bartholomew county, but not so much in Johnson and other counties. The top soils of these counties and parts of others like them, are very fertile and productive, and in seasons of normal rainfall and distribution never fail to produce well. It is different with clay loams and clay subsoils. With a proper underdrainage of these soils and with the right kind of cultivation, the moisture in seasons of short rainfall may be retained in the subsoil for use during tbe growing seasons. Scientific investigations have shown that for each pound of dry matter produced in growing wheat 400 pounds of water are required, and in corn 300 pounds of water is necessary for each pound of dry matter produced. These facts have beeu verified by experience as well as by scientific analysis. This season we have just now before us these facts verified by observation, the results of the dry conditions in May, and which support the facts of scientific analysis as to oats, that for every dry pound of matter in the production- of oats 500 pounds of water is required to mature a normal crop. As already stated, when the season has a normal rainfall, well distributed in the seasons of growth, all of our fertile soils produce well, because the grain crops are supplied with a due proportion of moisture to dry matter. The wheat plant requires its moisture in early fall and during the spring months, •ind as a rule nature affords such supply, for these are the months of greatest rain- with moisture, which is an important factor in plant growth. The two classes of soils mentioned, that with sand and gravel below, and that with a clay subsoil, are shown in the illustration on this page, which more fully illustrates the facts stated. Farm Home of J. L. Hewitt, Randolph County. fall, and even on porous subsoils the moisture is not leached away till the plant is well supplied. And no damage to wheat really comes from over dry seasons, unless at times in the fall, to start growth well before winter. It is not always so with oats, which requires the greatest quantity of water, for that crop is not seeded till March or April, and as we see this season, both April and May failed to afford the 500 pounds of water to the one pound of dry matter for a good crop. These facts as they apply to timothy and clover meadows are much the same as with wheat, both as they relate to the ra the proper surface manipulation of the soil to hold it. From what has already been stated it must be obvious that for all the grain crops it is well to break the surface soils dee, that are underlaid with clay subsoils, both for the purpose of avoiding stagnant water in contact with plants iu excessive wet seasons, and to utilize the moisture by capillary action in dry seasons. Wheat and oats do not root deep, but the moisture below, held by deep breaking, is valuable in dry seasons to these crops. The corn plant, however, is most benefited by holding the moisture iu this subsoil reservoir, for as TUX Figure 1. Shows dense character of clay sub-soil. Figure 2. Porous nature ofsand and gravel under the soil. tio of water to dry matter and to the distribution of rainfall in growing seasons. But with corn it is different. It requires 300 pounds of water to one of dry matter to produce it and the growth of corn occurs from May to August nearly inclusive, or the 90 to 100 days of the season of least rainfall. It is readily seen why in dry seasons, the corn crop is short, or fails in soils with sand and gravel below, for with such there can be no preservation of moisture as in clay subsoils, to be held and used by capillary action with already stated corn is grown during the months of least rainfall, and by the surface cultivation aud the dust mulch the moisture below is held for use of the plant. The economy of tile drainage is that of leaching the extra water through the surface soil aud thus sifting out and holding the fertility, and of removing the extra rainfall from the soil so as to prevent the stagnation which overcomes fertility in the growth of plants, and also for the purpose of admitting the aeration of the soil laden OUK NEIGHBORS. Editors Indiana Fsr__er: The older we grow the more are we convinced that we cannot get along vry well without friends and neighbors. We are dependent In many ways upon those about us and to a greater extent than most of us are willing to acknowledge. The social side of farm life is one that we cannot afford to neglect although at times our daily routine of labor seems to detract from this phase of our existence. Some oue has said when a farmer moves into a new community, if he is the right sort of a man ht* carries his neighbors with him. His own acts aud attitude to- wnnl others mark him as one in whom confident can or cannot be placed. If he is considerate his deeds are reflected by his neighbors and he soon becomes a well thought of and worthy member of the neighborhood. It doesn't always pay for neighbors to bo too confidential and chummy. Intimacy soon destroys the neighborly friendliness, because the whole thing is overdone, and in- the end, tlie erstwhile friends become enemies. It is a pretty serious thing when two near neighbors are not on speaking terms. When they pass on the road or meet elsewhere aud do not exchange greetings, both feel uncomfortable aud down deep in their hearts they wish it were otherwise. We can't afford to be without neighbors often it is better to overlook the petty annoyances and harsh sayings of a thoughtless neighbor than to quarrel with him aud lose him altogether, for no one is so iudependeut but what at times he must sock aid or beg a favor of another. The agricultural communities of our country is where we find the home of true Anglo Saxon democracy. It is fostered by the neighborly spirit which everywhere characterises this race. It makes ,for the best iu our American citizenship, and on this account the neighborly phase of our day sliould not be neglected. Of course some of our neighbors may not be up to the standard. There is the man who is always seeking the best side of a bargain and the one who is shiftless and is eternally borrowing from you, be it farming tools, or maybe grain to feed his half starved horses or cattle. Then there is the busy body who always knows a great deal about other people's affairs and tells more than he knows. Again is found in the neighborhood, the man who tries to keep his cattle and other live stock in fields with rickety, ill kept fences and whose animals are always giving you trouble in some form or other, and so it tfm's. The man who can keep on good terms with neighbors like these is certain- !;■ worthy of a hero's decoration. The best way to get on with some people is to have little or no dealing with the first; discourage the second at every good opportunity but in a diplomatic way; don't listen to the gpssip of the third and manage in some way either kindly or otherwise to have the fourth build good fences and keep li!3 stock within proper bounds. The farmer who deals squarely with his neighbors in every way never has lack of friends in the hour of need. H. S. C.
Object Description
Title | Indiana farmer, 1906, v. 61, no. 30 (July 28) |
Purdue Identification Number | INFA6130 |
Date of Original | 1906 |
Subjects (LCSH) |
Agriculture Farm management Horticulture Agricultural machinery |
Subjects (NALT) |
agriculture farm management horticulture agricultural machinery and equipment |
Genre | Periodical |
Call Number of Original | 630.5 In2 |
Location of Original | Hicks Repository |
Coverage | United States - Indiana |
Type | text |
Format | JP2 |
Language | eng |
Collection Title | Indiana Farmer |
Rights Statement | Content in the Indiana Farmer Collection is in the public domain (published before 1923) or lacks a known copyright holder. Digital images in the collection may be used for educational, non-commercial, or not-for-profit purposes. |
Repository | Purdue University Libraries |
Date Digitized | 2011-02-03 |
Digitization Information | Original scanned at 300 ppi on a Bookeye 3 scanner using internal software. Display images generated in CONTENTdm as JP2000s; file format for archival copy is uncompressed TIF format. |
Description
Title | Page 1 |
Subjects (LCSH) |
Agriculture Farm management Horticulture Agricultural machinery |
Subjects (NALT) |
agriculture farm management horticulture agricultural machinery and equipment |
Genre | Periodical |
Call Number of Original | 630.5 In2 |
Location of Original | Hicks Repository |
Coverage | Indiana |
Type | text |
Format | JP2 |
Language | eng |
Collection Title | Indiana Farmer |
Rights Statement | Content in the Indiana Farmer Collection is in the public domain (published before 1923) or lacks a known copyright holder. Digital images in the collection may be used for educational, non-commercial, or non-for-profit purposes. |
Repository | Purdue University Libraries |
Digitization Information | Orignal scanned at 300 ppi on a Bookeye 3 scanner using internal software. Display images generated in CONTENTdm as JP2000s; file format for archival copy is uncompressed TIF format. |
Transcript | VOL. LXI PUBLIC LIBRARY INDIANAPOLIS, JULY 28, 1906. NO. 30 SOILS AND QRUN CROPS. With Some Soils Everything Depends on Oiven Rain Pall. Conserving Moisture in Dry Seasons on Clay Subsoils. Moisture in Production. The following . hows the proportion of water to dry matter, grain aiid straw, in producing the crops named. 1. W heat 400 lbs. water to 1 lb of dry matter. Oats 500 lbs. water to lib. of dry matter. Corn 300 lbs water to 1 lb. of dry matter. Timothy and clover require I he same proportion of water to dry matter that wheat does to produce them. 2. 3. Scientific investigations have settled many primary considerations in crop trowing, and especially as regards grain crops. It is well to keep these well-settled facts in mind, as they relate to seasons, and soils and rainfall. When the season brings the normal rainfall and it ! is well distributed through the growing months of the cropping year, there is little or no uncertainty of crop-growing results on any of our soils. But when- the rainfall is below 28 to 30 inches a year, and not well distributed through the growing season, there is little help for the growing crops on the soils having sand and gravel beneath them, for upon such the moisture quickly leaches away and the plant is left helpless. With clay subsoils in such seasons it is different. Deep plowing leaves below it a reservoir which holds the moisture to be used by capillary action at the roots of the growing plants. The first mentioned soil formation, with porous conditions below, are found in several parts of Indiana, including a considerable area of Bartholomew county, but not so much in Johnson and other counties. The top soils of these counties and parts of others like them, are very fertile and productive, and in seasons of normal rainfall and distribution never fail to produce well. It is different with clay loams and clay subsoils. With a proper underdrainage of these soils and with the right kind of cultivation, the moisture in seasons of short rainfall may be retained in the subsoil for use during tbe growing seasons. Scientific investigations have shown that for each pound of dry matter produced in growing wheat 400 pounds of water are required, and in corn 300 pounds of water is necessary for each pound of dry matter produced. These facts have beeu verified by experience as well as by scientific analysis. This season we have just now before us these facts verified by observation, the results of the dry conditions in May, and which support the facts of scientific analysis as to oats, that for every dry pound of matter in the production- of oats 500 pounds of water is required to mature a normal crop. As already stated, when the season has a normal rainfall, well distributed in the seasons of growth, all of our fertile soils produce well, because the grain crops are supplied with a due proportion of moisture to dry matter. The wheat plant requires its moisture in early fall and during the spring months, •ind as a rule nature affords such supply, for these are the months of greatest rain- with moisture, which is an important factor in plant growth. The two classes of soils mentioned, that with sand and gravel below, and that with a clay subsoil, are shown in the illustration on this page, which more fully illustrates the facts stated. Farm Home of J. L. Hewitt, Randolph County. fall, and even on porous subsoils the moisture is not leached away till the plant is well supplied. And no damage to wheat really comes from over dry seasons, unless at times in the fall, to start growth well before winter. It is not always so with oats, which requires the greatest quantity of water, for that crop is not seeded till March or April, and as we see this season, both April and May failed to afford the 500 pounds of water to the one pound of dry matter for a good crop. These facts as they apply to timothy and clover meadows are much the same as with wheat, both as they relate to the ra the proper surface manipulation of the soil to hold it. From what has already been stated it must be obvious that for all the grain crops it is well to break the surface soils dee, that are underlaid with clay subsoils, both for the purpose of avoiding stagnant water in contact with plants iu excessive wet seasons, and to utilize the moisture by capillary action in dry seasons. Wheat and oats do not root deep, but the moisture below, held by deep breaking, is valuable in dry seasons to these crops. The corn plant, however, is most benefited by holding the moisture iu this subsoil reservoir, for as TUX Figure 1. Shows dense character of clay sub-soil. Figure 2. Porous nature ofsand and gravel under the soil. tio of water to dry matter and to the distribution of rainfall in growing seasons. But with corn it is different. It requires 300 pounds of water to one of dry matter to produce it and the growth of corn occurs from May to August nearly inclusive, or the 90 to 100 days of the season of least rainfall. It is readily seen why in dry seasons, the corn crop is short, or fails in soils with sand and gravel below, for with such there can be no preservation of moisture as in clay subsoils, to be held and used by capillary action with already stated corn is grown during the months of least rainfall, and by the surface cultivation aud the dust mulch the moisture below is held for use of the plant. The economy of tile drainage is that of leaching the extra water through the surface soil aud thus sifting out and holding the fertility, and of removing the extra rainfall from the soil so as to prevent the stagnation which overcomes fertility in the growth of plants, and also for the purpose of admitting the aeration of the soil laden OUK NEIGHBORS. Editors Indiana Fsr__er: The older we grow the more are we convinced that we cannot get along vry well without friends and neighbors. We are dependent In many ways upon those about us and to a greater extent than most of us are willing to acknowledge. The social side of farm life is one that we cannot afford to neglect although at times our daily routine of labor seems to detract from this phase of our existence. Some oue has said when a farmer moves into a new community, if he is the right sort of a man ht* carries his neighbors with him. His own acts aud attitude to- wnnl others mark him as one in whom confident can or cannot be placed. If he is considerate his deeds are reflected by his neighbors and he soon becomes a well thought of and worthy member of the neighborhood. It doesn't always pay for neighbors to bo too confidential and chummy. Intimacy soon destroys the neighborly friendliness, because the whole thing is overdone, and in- the end, tlie erstwhile friends become enemies. It is a pretty serious thing when two near neighbors are not on speaking terms. When they pass on the road or meet elsewhere aud do not exchange greetings, both feel uncomfortable aud down deep in their hearts they wish it were otherwise. We can't afford to be without neighbors often it is better to overlook the petty annoyances and harsh sayings of a thoughtless neighbor than to quarrel with him aud lose him altogether, for no one is so iudependeut but what at times he must sock aid or beg a favor of another. The agricultural communities of our country is where we find the home of true Anglo Saxon democracy. It is fostered by the neighborly spirit which everywhere characterises this race. It makes ,for the best iu our American citizenship, and on this account the neighborly phase of our day sliould not be neglected. Of course some of our neighbors may not be up to the standard. There is the man who is always seeking the best side of a bargain and the one who is shiftless and is eternally borrowing from you, be it farming tools, or maybe grain to feed his half starved horses or cattle. Then there is the busy body who always knows a great deal about other people's affairs and tells more than he knows. Again is found in the neighborhood, the man who tries to keep his cattle and other live stock in fields with rickety, ill kept fences and whose animals are always giving you trouble in some form or other, and so it tfm's. The man who can keep on good terms with neighbors like these is certain- !;■ worthy of a hero's decoration. The best way to get on with some people is to have little or no dealing with the first; discourage the second at every good opportunity but in a diplomatic way; don't listen to the gpssip of the third and manage in some way either kindly or otherwise to have the fourth build good fences and keep li!3 stock within proper bounds. The farmer who deals squarely with his neighbors in every way never has lack of friends in the hour of need. H. S. C. |
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