Drilling Fine Limestone for Legumes
THE IMPORTANCE OF LIMESTONE as a soil treatment, especially for legumes, has come to be widely appreciated, but its use has not become a general practice. The labor required to deliver and to apply two or more tons of 10 mesh material per acre is often too large to fit into the farm scheme except at periods of slack labor. Moreover, the maximum effectiveness of this coarsely ground material is delayed until six months or a year after its application. Finally, the wide variation in the quality of such stone available, especially in its content of material fine enough to pass a 40 mesh sieve and be effective during the first season, gives a correspondingly wide range in its effectiveness and in amounts necessary for good results. All these are handicaps in the wider adoption of liming as a regular farm practice and they have pointed to the need for a simpler method. This has been found in the plan of drilling smaller amounts of the more finely ground limestone with the seeding of legumes. It should not be understood that the plan of using larger amounts of ordinary limestone is not as valuable as ever, but the use of time limestone permits liming under many conditions where heavy liming is not commonly practiced.
According to the common conception of the function of limestone, it is applied to the soil as a means of removing, or correcting, soil acidity. Experimental studies at the Missouri Experiment Station, however, show that limestone, or calcium carbonate, renders two services. One of these is the removal of the soil acidity that is accomplished by the carbonate part. The other is that of supplying calcium as a nutrient to the plants. In the past, emphasis on the removal of acidity has so completely overshadowed the importance of supplying the much needed calcium for plants, that this latter function of lime has not been fully appreciated. Experiments have shown, however, that in terms of better plant growth, the application of calcium to the soil is more important than the removal of acidity. Compounds of calcium other than its carbonate, which do not remove soil acidity, will often serve in place of limestone. Conversely, however, carbonate compounds that will remove the acidity but do not contain calcium do not have significant influence on plant growth. Since limestone is the cheapest source of both calcium and carbonate, such other compounds have not been substituted for it and these facts were not observed in practice. Thus, in using calcium carbonate to remove the soil acidity, the calcium needs of the plant have nevertheless been met without ascribing to the limestone application for this particular and important function.
Studies on calcium as an important nutrient for legumes have shown that the amount of this element required by these plants is large in comparison with the needs of non-legume plants. For 25 bushels of wheat and a ton of straw, only 5 pounds of calcium are needed. For 50 bushels of corn and a ton of fodder a like amount must be provided. To produce two tons of clover hay—about the crop that might be expected on 50 bushel corn land—the soil must supply 80 pounds, or 16 times as much calcium. A two-ton hay crop of soybeans, often considered able to grow on sour soil, requires 55 pounds of calcium. Legumes make large demands on the soil for calcium in comparison with other crops, and for this reason they represent the first group of crops to show disaster from a depleted supply of calcium in the soil.
In terms of the amount of limestone required to supply this required calcium, however, the figure is small. Pure limestone contains 40% calcium, or 40 pounds per hundred, hence a crop of 50 bushels of corn and stover would take calcium from the soil, equivalent of only 12 1/2 pounds of limestone. Red clover, a much heavier feeder on calcium, would take for a two-ton crop, the calcium that would be supplied by 200 pounds of pure limestone. Soybeans at the same acre yield would need about 150 pounds. Thus the actual calcium needs of the crop can be supplied in relatively small quantities of limestone if it can be delivered to the plants in such a way that they can use it fully. In respect to the crop needs of calcium, therefore, we may think of limestone in terms of pounds rather than tons, provided this is delivered to the plant in usable form.
When the limestone needs approach such small figures per acre the liming treatment becomes similar to that of applying fertilizer. Then, too, since it becomes a matter of getting the lime, or calcium into the plant, it further approaches fertilizer in the matter of providing limestone of ready solubility. Limestone is similar to fertilizer in still another respect, namely, that the effects of the lime are marked in the early life of the plant. Experiments have shown that legume plants given lime are larger and more able to take nutrients from the soil in their early life, when given access to lime for only the first ten days of their growth and then transplanted as seedlings to acid soil, than when lime is withheld. Also they are more active in forming root nodules and earlier as well as superior in nitrogen fixation.
As a rock, limestone is usually considered insoluble, yet this is not the whole truth when one recalls the numerous caves dissolved out of limestone by running water. When finely ground, of course, limestone becomes more soluble in the same way that powdered sugar dissolves more quickly than rock candy, yet both are the same chemical composition. When limestone is ground into a powder that is fine enough to pass a sieve with 100 holes per linear inch, or 10,000 holes to a square inch, its action in the soil is practically as rapid as that of the water soluble forms of lime, namely, quick lime and hydrated lime. The finer grinding of limestone with this resulting increase in solubility make it behave like a fertilizer in speedy effects.
By drilling finely ground limestone into the soil at the time of seeding the crop, the approach to fertilizer is still closer in method of application and in use by the small plants in their first stages of growth. The effectiveness in starting legumes by drilling these smaller amounts which do not remove the acidity of the entire soil layer, points to the fact that it is not necessary to correct all the soil acidity before legumes can be grown. Finely ground limestone has started sweet clover on soil whose degree of acidity was quite high, (pH 4.9, requiring more than two tons of coarse limestone on a silt loam), and this acidity was slightly changed in no greater distance than two inches from the drilled stone. Even with heavy applications of limestone, legumes succeed when not all the soil acidity has been removed. In fact it has often been observed that clover will succeed in consequence of applications of coarse limestone on soil whose test after treatments still shows considerable acidity. Such soils are evidently delivering enough calcium to the plant for successful growth even though they are still acid. When plants can be transplanted from limed to sour soil and are better there because of the short early period in the presence of limed soil, and when nodules are produced in the soil at some distance from the streak of limestone applied by the drill, as has been common observation, it is clearly evident that lime can serve the plants without neutralizing the acidity in the entire soil area. It is highly probable that it would be disastrous to plant growth in other respects if many soils were suddenly neutralized completely. Potato scab is encouraged by neutral soils and the potato grower may well consider fine liming as a means of growing legumes for organic matter addition to his soil without bringing on the scab disease that results from correcting the acidity completely. Excessive liming has given bad effects in a sufficient number of cases to lead us to believe that some degree of acidity is desirable. Under such circumstances limestone behaves as a fertilizer in that it supplies the calcium needed by the plants, and can be handled on this basis in farm practice on many soils without necessarily completely neutralizing the soil.
If limestone is to be rapid in its action it must be finely ground. Much pulverized, or powdered, stone is now available as a consequence of improved methods of separating this fraction during grinding. Likewise channels that formerly consumed such output are now using less, so that it is available at prices more conducive to agricultural use. Some quarries are providing stone of such fineness that all of it passes the 100 mesh screen, while many have 40 mesh, or 30 mesh, stone. These latter contain no particles larger than those which will pass screens of such size and usually have about one-half, by weight, fine enough to pass the 100 mesh screen. These also lend themselves to drilling better than the 100 mesh material which does not flow through machinery easily.
The regular 10 mesh stone commonly broadcast at heavy rates might also be drilled according to this plan but it contains such a small portion of finely ground powdered stone that it is slower in its action. If larger amounts can be drilled so as to put into the soil as much powdered stone as is added by the finer material, similar results may be expected. Such large amounts cannot be handled so easily through the drill, nor with so little wear on the machinery. It seems doubtful economy to drill the coarser stone in place of the 40 mesh and finer material. For drilling purposes and effective results the finer stone should be considered.
Beside limestone, there are other compounds which can supply calcium and are often available. Acetylene plant waste is a form of very finely powdered lime hydrate that on drying and exposure to air will change to calcium carbonate. It will serve effectively as limestone, though its fluffy nature prohibits easy drilling unless there is an agitator in the drill box. Lime tailings, residues from burning lime, are another by-product that deserves consideration. Lime hydrate in the commercial form will also serve. It carries as much calcium in 74 pounds as limestone does in 100 and one will need only three-fourths as much of this as of limestone. Granulated quicklime may also be used, but is not as convenient to handle because of its caustic nature and like the hydrate may disturb germination if put into close contact with the seed in the soil. About 56 pounds of this are equivalent in calcium value to 100 pounds of limestone. When quicklime air slakes completely and changes from the stone to the powder form, it may also be used. Then it has no weight advantage and 100 pounds are required for the equivalent of 100 pounds of limestone. It also has the same chemical composition. Its fineness introduces difficulties in drilling it effectively. Other kinds of lime and lime wastes may be considered and can be evaluated on basis of their calcium supplying power. Many of these miscellaneous forms of lime deserve more consideration as a soil treatment.
If smaller amounts of finely ground limestone are to be successful in supplying plants with calcium and establishing the crop, the limestone should be drilled into the soil. Broadcasting such small amounts as 500 pounds per acre is not significant in its effects. Yet when this same amount is drilled, each drill row represents small soil areas where the limestone is concentrated and the soil along the row is more highly saturated with lime. Experimental studies show that the higher the degree of saturation of the soil by lime, the more readily does the plant secure the lime. Thus, the plants find in the drill row this favorable condition for supplying lime and will grow there. As is true for wheat and other drilled grains, so it is true for legumes—their establishment in the drill row only usually means plenty of plants per acre and a good stand.
Finely ground limestone need not be drilled deeply. It moves slightly downward in its reaction with the soil. Even if put right on top, it will be fairly effective but in this case the wind scatters it to reduce its effects. It is unnecessary, however, to make the drilling operation a heavy load by setting the drill deeply into the soil. If a quiet or non-windy time is chosen, the drill can be run shallow, the limestone delivered in a very narrow strip into the soil with light cover, and narrow, highly-loaded streaks of soil through the field provided. There the plants can early find their needed lime supply and get off to a good start. This early growth is essential in the life of the clovers if they are to get their roots down into the lower soil and establish themselves in competition with the nurse crop of wheat or oats for the soil fertility and moisture. Only as they do so can they survive the summer and make a paying crop later. Lighter applications of limestone cannot be promptly beneficial if scattered enough through the entire surface soil. They can be helpful, however, if drilled into the soil.
Since fine limestone is considered much like a fertilizer, naturally the season for drilling it might be expected to be that time when the legumes are seeded. It has been found a good practice to drill the limestone in the spring when the clovers and other lime-loving legumes are sown. The fertilizer attachment of the grain drill will deliver the limestone, while the grass seed attachment delivers the seed. In this way one operation over the field completes the seeding. If the drill is not run into the soil deeply, the seed may be delivered down the spout and the seeds and limestone put into immediate contact. If the seeds are covered too deeply by soil or heavy droppings of the dry powdered stone, the germination and stand may be disturbed. The seed delivery spouts on the drill may be detached from the sprouts leading down to the drill shoe, and the clover seed scattered on the surface of the soil. The seed spouts may also be extended to scatter them behind the drill, where they will fall into the drill furrows immediately over the limestone and be covered well enough by the first rain.
When drilling the fine limestone in the spring season, it should be done as early as possible because of the well known need for seeding clover early. This is sometimes impossible because the soil is too wet to permit going over it with the drill, and the wait for suitable soil conditions delays the seeding until the nurse crop is so large that the clover will be smothered out, or fail because of moisture shortage. It is not necessary that the limestone and the seed go on together, provided the soil is not cultivated or disturbed between these two operations. Consequently, the fine limestone may be drilled during the winter when soil conditions permit. The broadcast clover seeding may follow at the proper date. This will serve practically as well as drilling the two together.
As heavy applications of coarse limestone are often made in connection with wheat seeding in the fall, so the drilling of the finer limestone may also be done at this season. The limestone may be drilled like a fertilizer directly with the wheat. Since the wheat and limestone cannot be mixed and seeded together through the grain section of the drill very successfully, the stone should be put on with the fertilizer attachment. Limestone so applied in the fall will be effective the following early spring when the clover is seeded broadcast in the customary manner. If fertilizer is to be applied for the wheat this may be mixed with the limestone and both put on at the same time. Such a mixture may also be drilled with the clover seedings. There is no serious danger from the interference of one with the other. On the contrary, there may be improvement in the effect of the fertilizer as a result of the presence of the limestone. Likewise, for the limestone effect on the wheat, this will not be detrimental but may be helpful. Inoculated soil may also be mixed with the limestone as a means of inoculating the following clover seeding.
As for the time when fine limestone may be drilled most conveniently and effectively, the fall seeding season is a good one where wheat or barley is the nurse crop. If oats serves as such, the limestone may be drilled similarly with the oats in the spring and the clover broadcast later. When the legumes are seeded alone, then the limestone may well be drilled at their seeding season.
“How long will the fine limestone last?” is a common question when one contrasts this method with that of broadcasting a heavy application of coarse material that is effective to the legume crops in more than one round of the rotation. Legumes are the first among the crops to need lime, consequently, the fine stone is drilled with the legumes. The effect will last longer than this one crop if the soil is not disturbed. Sweet clover has reseeded itself after a start with fine lime, showing that the effect can carry over to the third year. When only the small soil areas represented by the drill rows are treated and the ground plowed afterward this small amount of limed soil is too thoroughly scattered through the great soil mass to lend much effect. When the next legume crop comes around in the rotation another limestone treatment should be used. Because broadcast heavy liming is an arduous task and represents a significant investment, one naturally hopes that its effects will last a longer time than for one single year of rotation. Drilling the fine lime is a simple, one-man operation of moderate cash outlay and it might be considered as a part of the treatment for every legume seeding.
The most effective method of drilling fine limestone is by means of the fertilizer attachment on the grain drill. This will handle limestone effectively though one cannot expect even this machine to operate without attention. One must always make sure that the stone is not failing to get down into the distributing machinery satisfactorily. It is also necessary to learn the rate of delivery. Some careful tests have shown that very fine limestone was delivered at only three-fourths of the rate as given for the particular set of gears and gate opening specified for that of fertilizer. If one is to drill 500 pounds of the finer stone it may be necessary to set the machinery at a higher figure than that for fertilizer delivery.
The ordinary grain drill without fertilizer will distribute fine limestone if some agitating device is used. Some grain drills are already made for, and can easily be equipped with, an agitator in the grain box so that they will serve to drill fine limestone. In testing such a machine with 100 mesh limestone, it delivered 200 pounds per acre when set for six pecks of oats, and 350 pounds per acre when set for 12 pecks. Another drill equipped with a home-made agitator tripped by a block on the wheel, delivered slightly less than 300 pounds when set for 9 pecks of oats. Such machinery is not as convenient as the fertilizer section of a grain drill, but will serve and can be used to drill the stone. As coarser stone is used, the wear will be greater, but this is not a serious matter and should not prohibit drilling limestone by this method. It is important, however, that the drill be cleaned thoroughly thereafter.
As the declining fertility of our soils becomes more widely recognized and the use of fertilizers to replace it becomes a more general practice, the fertilizer drill will be a more common machine for applying limestone as well. In respect to farm machinery, the fine limestone drilling methods will fit into the already common stock of farm equipment and call for no special machinery of limited use.
It is not uncommon experience in Missouri to find that an application of limestone alone does not secure a stand of clover. This has been true with heavy applications of limestone, but has come under more careful observation and with more emphasis in trials with fine limestone in conjunction with fertilizer treatments. Clover requires more than limestone for its successful stand and growth. It is true that liming increases root nodule production and, through the nodular bacteria, helps the plant to get its nitrogen from the unlimited supply in the soil air. In respect to this one nutrient, beside calcium, liming increases the supply of nitrogen for the legume plants by their improved nitrogen fixation. Limestone cannot substitute, however, for soil shortages in phosphorus, potassium, moisture or any other items required for plant growth. The addition of phosphorus to limestone has shown itself beneficial. The addition of potash is also noticeable in its effects so that on many soils of the state, the level of this nutrient is so low as to deserve consideration. Farm manure will supply some of this shortage and should often be used for this reason in conjunction with liming for a legume stand. Resistance to drought by clover was increased as limestone was supplemented with other treatments, possibly because these produce greater plant vigor and a deeper tap root. These illustrations indicate that more liming is often required, and that if fine limestone has been drilled with the clover seeding which fails, that failure should not be wholly ascribed to the fault of the fine liming method. Rather, some other soil deficiency may be responsible. The fine liming method will supply the needed calcium, and will increase nodule production and consequent nitrogen fixation, but it cannot take the place of other requisites for this crop. When used alone fine lime should not always be considered as a guarantee for a good stand and crop of clover.
As the soils in the regions of great rainfall and heavier crop production have become low in lime—now being especially recognized by clover failures—so have they also become correspondingly low in other nutrients not so grossly removed by plants. The soil deficiency in these is just as disastrous since the crop is impossible unless each of the required nutrients is amply supplied. The use of fine lime drilled with wheat has sometimes improved the wheat crop, pointing out that the soil was low in calcium even for wheat, and doubtless for corn and other crops that require but small amounts of it. Liming ahead of corn has improved this crop, probably by indirect as well as by direct effects through the calcium supplied. Oats have sometimes been improved by liming and reports of improvement in soybeans from limestone drilled with them are not uncommon. Its benefit on oats and wheat nurse crops, suggest similar effects from it on barley serving the same purpose, especially since barley is the most sensitive of the small grains to the lack of lime. The low supply of lime that may be disastrous to the extent of complete crop failure for legumes, is therefore injurious to many other crops.
This declining supply of soil fertility may be responsible for clover failure where it is grown with a nurse crop as contrasted to success where grown alone. The fertility supply of the soil may not be sufficient for two crops. Illustrations are not uncommon of clover in wheat drilled around shocks of corn fodder. In such cases the clover may be large next to the shock where nutrients were leached from the fodder into the soil by rain, while farther from the shock where no wheat was drilled and the clover grew alone it will be somewhat smaller. It will usually be still smaller within the wheat crop. The improved growth of clover around the shock from which the added fertility was leached into the soil, points out that the fertility of the soil is low for clover, but especially so when it must grow in competition with the wheat for this limited fertility supply. Farm experience in growing clover alone successfully is testifying to this situation. When grass takes alfalfa, this is also a testimony that the fertility level will not meet the high demands for good alfalfa that would smother the grass. We are expecting too much of many soils when we seed a nurse crop and clover too, and expect both to succeed on the low level of soil fertility offered them.
This declining fertility level is evident in spite of the fact that a liming treatment, especially a heavy application, helps much in making other plant foods more effective. It is now known that liming helps the plants to obtain more potassium. Also it is instrumental in making a phosphorus treatment more beneficial. On limed land phosphorus is usually more effective than on unlimed soil. Lime also helps the plant to get nitrogen. It aids the plant in making much better use of the limited supplies of these other nutrients. It does not add these to the soil, hence the already low supply will be more rapidly depleted by liming. If, however, clovers can be grown and larger crop yields result, the restoration of the fertility should be quickly undertaken when this soil need is fully appreciated. As we use more limestone, attention must likewise be given to other deficiencies of soil fertility which this practice will help bring to our notice, and for which limestone cannot be a substitute.
To date the drilling of the finer limestone has been tried with successful results by farmer cooperators in many parts of the state. The soil types represented include the following: Boone, Cherokee, Crawford, Decatur, Edina, Gerald, Grundy, Knox, Lebanon, Marshall, Memphis, Oswego, Putnam and Summit silt loams; the Shelby and Lindley loams; Clarksville and Baxter gravelly loams; Lintonia fine sandy loam; and Wabash clay loam. By no means have all soil types been included in this rather extensive list, but those of level topography, heavier subsoil and significant degree of acidity have been grown to acid sensitive crops by means of lighter applications of limestone drilled on them. They testify to the success of this practice on those soils most difficult to seed to clover. Not only red clover, but sweet clover, and in some cases, alfalfa has been started by this treatment. Unfortunately, liming cannot offset bad seed, summer drought or infertility, but it can care for the calcium deficiency, or lime need, on many of the prevailing soil types in the state.
In terms of cost of the limestone, the drilling of a quarter ton of finer limestone is less than that of broadcasting two tons of 10 mesh material per acre. With the price of the former at $5.00 per ton at the quarry and a delivery charge of $1.00 per ton within a radius approaching a hundred miles. A 500 pound, or quarter ton application should call for a cash outlay of $1.50 per acre. For two tons of 10 mesh material such a cash outlay would allow only 75 cents per ton delivered on the farm. Costs of this coarser material have usually been much greater than this, so that drilling finer limestone should not exceed—and will usually be less than—the per acre cost of coarser material at the two ton rate.
In terms of the labor of distribution, the drilling method effects a real saving. To drill 500 pounds per acre on 20 acres is a one-man labor load, totaling five tons of material, while the corresponding labor load of 40 tons broadcast might require the help of the neighbors. It is this labor requirement that should be considered as the significant advantage of the finer limestone, and that makes this method lend itself to bringing limestone to soils where the other method might mean too great an initial cost. The smaller amount of limestone means less initial cash outlay; it permits the stone to be hauled to greater distance from railroads or delivery points, and makes possible liming within the farmer’s own labor. The one-man labor load and smaller amounts of stone required make delivery possible at any time with storage for later use. When its use becomes more widespread, the stone may be stocked more generally by local dealers and thus still greater economies effected. Under such conditions, its costs when used regularly in every rotation should not exceed the costs of heavier applications of coarser stone applied less often.
This method of handling the liming need of the soil reduces it from a complex problem of large cash outlay and extensive labor, to a regular farming practice that can be geared into the routine farm program without its disruption. On such a basis the drilling of fine limestone may be accepted as a regular part of the legume seeding whenever it comes around in the rotation just as fertilizing should be a part of wheat seeding. Under such conditions more legumes can be successfully grown, more fertility restored to the soils and higher profits returned by the land.