By Dr. William A. Albrecht

Summary: A comprehensive discussion of the amazing role of calcium in the soil and its effect on crops and animals, written by one of the greatest soil scientists of all time. Dr. William Albrecht, who chaired the soils department at the University of Missouri College of Agriculture, is known in the organic farming movement as the “father of soil fertility research.” Born in 1888, he published his first article on soil fertility in 1918 and would publish research papers continually until his death in 1974. Albrecht was a friend of Dr. Royal Lee, and the Lee Foundation published several of his papers available in this archive. From The Land magazine, 1943. Lee Foundation for Nutritional Research reprint 8.

The following is a transcription of the original Archives document. To view or download the original document, click here.


Calcium is at the head of the list of the strictly soilborne elements required in the nourishment of life. It is demanded by animal and human bodies in larger percentages of total diet than any other element. Its own properties—such as, for example, its relative solubility in some forms, its pronounced insolubility in others, its ease of displacement from rock and soils by many elements less essential, and the multitudinous compounds it forms—all make it the mobile one of the Earth’s nutrient ions.

These properties are responsible for its threatening absence from our surface soils that are bathed in the pure water of rainfall and for its presence in the water at greater soil depths in the distressing amounts that make it appear as stone in the teakettle or as post-bathing rings in the bathtub.

These same properties that seemingly impose shortages and hardships have given cubic mile upon cubic mile of limestone in geologic sea deposits later uplifted as land areas widely distributed in close proximity to the soils now suffering shortages of calcium needed for plant and animal nutrition.

While calcium is moving by aqueous aid in this cycle from the surface soil of our land to the sea and back to our soils again, this very nomadic habit makes possible its services in nourishing life. As in other natural performances, it does its work while running downhill. If maximum benefits to life are to accrue while this natural cycle continues, we must understand it and help to fit life into it.

An understanding of calcium and its role in the nutrition of life is the start in getting acquainted with the first on the list of all the soil-given elements. Its behavior [can] be profitably elucidated through the help of our observations of animals, animal assay methods, and other biochemical behaviors. When all the other soil-given elements are similarly studied, they will no longer remain micronutrients beyond our general understanding—as they must when the research light has no more candlepower than that of simple chemical analysis. Calcium may well be the “test case” or “pilot plant” experience to guide our thinking and understanding of all the other nutrient elements of the soil for the nutrition of microbes, plants, and animals.

Chemistry has long been the science of analysis. Nature has presented herself as something to be examined, to be taken apart, and to have its parts measured, named, and classified. Functional significance of each part has been assigned as fast as experimental procedure could study each as a single variable while all others are held constant. Only recently has chemistry become the science of synthesis. Its synthetic efforts are now giving us dyes in manifold colors and fibers of rayon and nylon for fabrics that fairly rival the rainbow itself. Nutritional minerals and medicinal compounds as complex as the vitamins themselves are now products of the chemist’s skill.

Nevertheless, nutritional studies still move forward mainly on the pattern of analytical procedures. Many are the parts and the factors in nutrition that remain unknown. We are still wondering how many golden eggs can be laid by that great goose known as nature. The list of carbohydrates, proteins, fats, minerals, and vitamins has had increasing numbers of compounds within each to be given particular emphasis. A dozen or more minerals coming from the soil [have shown] importance far beyond the magnitude each of them represents as a percentage of the body composition or of our daily diet. The vitamins—of recent recognition as essentials on the dietary list—have already increased in number [toward] a total of about fifty [that] is certainly going to drive many people to the drugstore. Three specific fatty acids are now listed, and some thirty amino acids must be ingested if nutrition is to be without some health troubles.

Synthesis has not yet been much used as a technique to help in our understanding of biological behaviors. We have not yet formulated the ideal toward which we are striving because normal bodies and good or perfect health are yet widely unattained. The analytical procedures and single-element controls are still in vogue, unsatisfactory though they may be. The isolation of one essential compound and the demonstration of its essentiality by the abnormalities its absence invokes is still the main procedure in nutritional studies. Plant physiology, likewise, demonstrates the plant troubles [that occur] when, for example, the calcium supply is varied, or when phosphorus is reduced, or when either is completely withheld. All the separate items on the essentials list have had their individual effects demonstrated, and we are mapping the world in terms of their individual absences. Little has been done, however, to vary two or three elements at the same time. The number of combinations would run the experimental trials into legion, and consequently such experiments have not yet been undertaken extensively.

But such multiple variations are the situations in nature, where all the soil-given nutrients, for example, may be varying during the life or growth cycle of a single organism. It is impossible therefore in natural performances to segregate the effects of separate elements. They can be evaluated only as a summation in terms of the final plant or animal. It is for this reason that we must resort to the bioassay method. It becomes necessary to use the animals themselves to obtain more-gross results of value in terms of our own life before all of the intricate individual processes can be learned and life itself synthesized thereby.


Nutritional thinking, however, is moving forward rapidly. It is not limited to compounds such as the carbohydrates or proteins and the chemical reactions they undergo. It is giving detailed attention to the catalysts that speed these reactions—if vitamins can be considered in this category. Body catalysts for improved mineral management, such as thyroxin from the thyroid gland and the activities of the parathyroid in control of the calcium and phosphorus in storage and in circulation, are bringing into the limelight the importance of supplies of these elements as well as their catalysts.

Calcium behavior in nutrition is no exception to this concept of complex interrelation; its supplies in the bones, the bloodstream, and the alimentary tract may be moved through this series in either direction according to certain relations of its amounts to the supplies of the catalyst exercising control, vitamin D. And given that there are a dozen soil-given elements, each with its variable supplies and possible catalyzed behaviors to be synchronized, the possibilities for shortages or deficiencies multiply themselves quickly. Attention to calcium can be in terms only of its deficiencies as gross manifestations when all of its many functions are not yet catalogued.

Soil is formed from rocks and minerals by the climatic forces of rainfall and temperature. The presence or absence of calcium in the soil has long been the soil scientist’s index of the degree to which the soil has been developed or to which the rocks have moved towards solution. As rocks are broken down to form soil by increasing but not large amounts of rainfall, there is an increase in the soil’s content of active calcium. Then, as the amounts of rainfall go higher and temperature increases, there is calcium depletion. Life forms—whether of the lower, such as the microbes, or of the higher, such as plants and animals—all are part of this calcium picture.

The distribution of the different plants and animals as well as their densities of population take their ecological pattern very much according to the calcium supply. The United States divides readily into East and the West according to the lime content of the soil. The dividing line across the central United States puts lime-rich soils to the west and calcium-deficient soils to the east. This is according to the lesser amounts of rainfall to the west and the higher rainfalls and temperatures to the east—these differences having been so related as to weather the soils just enough to leave those in the West with calcium and to carry the weathering to the point of the removal of calcium in the East. Higher temperatures and rainfall, as [is found] in the Southeast, not only remove the calcium but change the clay complex, so that it has little holding or exchanging capacity for any of the soil mineral elements.

In these facts there is the basic reason for calcium deficiency and many other deficiencies in the humid tropics. Here is the basic reason for the confinement of the population of the wet tropics mainly to the seashores, where fish return the flow of soil fertility, in part, from the sea back to the land. Such facts account for the sparsity of population in the humid tropics, and yet we marvel at the tremendous vegetative growth of jungle densities. We forget that the jungle’s contribution for human use is mainly wood or fruits, which, if not actually poisonous, have little food value and at best only drug value, as [in] coffee, cinchona, and the alkaloids. It is this larger soil picture—with its highlights of calcium presence and its shadows of calcium absence—that makes the pattern to which all life, whether microbe, plant, animal, or man, must conform.

Microbes, as the agencies of decay, testify to the level of the nutritional conditions by the rates of destruction of the debris that they rot or on which they feed. Pine needles decay slowly because they are grown on a calcium-deficient soil and are consequently deficient in this element essential in the diet of microbes and in all the nutritive values associated with calcium in plants. Timothy hay and timothy sod decay slowly. Clover hay and clover sod rot quickly. “Clover and alfalfa hays,” says the farmer, “are hard to make because they spoil so quickly.” This is merely saying that such hays, as products of soils rich in calcium and therefore themselves rich in this element, allow the bacteria to multiply faster, or nourish themselves better. Consequently, the bacteria consume clover and alfalfa hays more rapidly than they consume timothy or pine needles. Cattle choices agree with the microbial choices.

Rapid decay of certain substances points to these as balanced foods for microbes and is an index of chemical composition and nutritional value for higher life forms that we too often fail to appreciate. We have been thinking [solely] of the disappearance of debris as it rots and have not been measuring the growth of the microbial crop. Microbes, as a kind of guinea pig for quick evaluation of the dietary contributions of the substances on which they feed, offer a neglected scientific technique for judging much that might be considered human food. Insects can serve likewise. If neither microbes nor bugs care for certain substances, should these be considered as of food value for higher life forms? Whole wheat flour “gets buggy” so much more readily than white flour, and by just that much is it [not] a more wholesome food?

Calcium for microbes in the soil’s service as a plant food factory has only recently become appreciated. Legumes cooperate with nodule bacteria for the appropriation of nitrogen from the air in many soils only when calcium is supplied as lime. Not only the plant but the legume microbe too makes high demands for calcium. The microbe separated from the plant must be given liberal supplies of calcium if this cooperative struggle for nitrogen, or protein, is to be successful.


Microbial decay processes within the soil by which nitrogen, as ammonia, is converted into nitrate also depend on the calcium supplied. Unless the clay of the soil, for example, has calcium present in liberal amounts, this conversion of nitrogen does not proceed rapidly.

The function of calcium [in making] the phosphorus of the soil more effective was [first] suggested [to scientists] by microbial behaviors. With calcium and phosphorus absorbed on a clay medium, the growth of certain microbes made the medium acid, while other but closely similar microbes made it alkaline. This difference occurred because both calcium and phosphorus are brought off the clay and into solution, with the result that intermittently one or the other of these dominates over the other—phosphorus dominating to make the medium acid, calcium dominating to make it alkaline.

Microbes apparently separate both calcium and phosphorus at the same time from the absorption forces of the clay but consume one or the other differently after this separation, to bring about the acidity or the alkalinity. Here are calcium and phosphorus in the microbial diet, and here they are closely associated in their nutritional services—just as they are found associated in plants and just as they function together in animals, mainly as the compounds of the different calcium phosphates.

Microbial nutrition suggests itself as an indicator of soil fertility and therefore of plant and animal nutrition. Microbes, as they grow rapidly and rot vegetation quickly—or conversely as they grow slowly and rot it slowly—indicate the soil nutrient supply by revealing the composition of the products grown by that soil. Pine needles decay slowly, and oak leaves decay slowly, but elm, linden, and other soft-wood leaves decay rapidly.

The Swiss farmer selects leaves for bedding litter for his cows and goats from the portion of the forest with the soft-wood trees because these leaves rot more completely in the manure than oak leaves do. The service of the leaves in decay, when mixed with animal excrement, and in the return of their nutrients to nourish the grass is judged by the Swiss farmer through this microbial indicator. The rate of decay can be taken as a universal indicator of the nutrient balance for microbes and therefore as balance for higher life forms.

The organic matter produced on a soil and going back into the soil reflects, by its rate of decay, the plant composition and therefore the fertility of the soil producing it. The size of the microbial crop, as reflected by its activity and like any other vegetation, is determined by the nutrients being mobilized in the soil. If calcium is deficient there, then the organic matter grows with a less proteinaceous composition or is mainly of carbonaceous content. Such vegetation makes a poor microbial diet. It reflects this fact when it accumulates or remains for a longer time, while the proteinaceous, or more calcium-rich, vegetation decays more rapidly.

The microbes, as lower plant forms, give us the ecological pattern of higher plants that serve to nourish higher animal forms. They point out, in general, that the vegetation produced on soils amply supplied with calcium is mineral-rich and proteinaceous, to serve the microbes well in their nutrition. On soils deficient in calcium, the vegetation is carbonaceous, protein-deficient, mineral-deficient, and lacking in many organic and mineral complexes requisite not only for microbes but for the higher life forms as well.

Microbes give us this larger ecological picture, in agreement with the soil map of the United States. Prairie soils or calcareous soils, with their proteinaceous and mineral-rich vegetation, are in the West, and forest soils and carbonaceous vegetation are in the East. Calcium is the index factor associated with these differences; as a very helpful factor, it needs to be given recognition and attention in connection with the larger picture of crops and foods of correspondingly variable nutritional values produced on these different soils.


The delayed appreciation of the significance of calcium in plant nutrition may be laid at the doorstep of a confused thinking about liming and soil acidity. The absence of lime in many soils of the non-temperate zone has long been known. Lime in different forms, such as chalk, marl, gypsum, or land plaster, has been a soil treatment for centuries. Lime was used in Rome in BC times, and the Romans used it in England in the first century AD. Chalking the land is an old practice in the British Isles. Calcareous deposits such as “The White Cliffs of Dover” were appreciated in soil improvement for centuries before they were commemorated in song.

Liming the soil is a very ancient art but a very recent science of agriculture. It was when Leibig, Lawes and Gilbert, and other scientists began to focus attention on the soil as a source of chemical elements for plant nutrition that nitrogen, soluble phosphate, and potassium became our first fertilizers. It was then that the element calcium and the practice of liming were put into the background. Unfortunately for the wider appreciation of calcium, this element, in the form of gypsum, was regularly a large part of the acid phosphate that was applied extensively in fertilizer to deliver phosphorus. Strange as it may seem, superphosphate fertilizer carries more calcium than it does phosphorus, and consequently calcium has been used so anonymously or incidentally that its services have not been appreciated.

While fertilizers held our thought, calcium was an unnoticed concomitant. Yet it was doing much for which the other parts of the fertilizers were getting credit. Appreciation of the true significance of calcium in plant nutrition was therefore long delayed.

More recently, soil acidity has held attention. This, again, has kept calcium out of the picture. Credit for the service of liming has been going to the carbonates with which calcium is associated in limestone. It was a case of a common fallacy in reasoning, namely the ascribing of causal significance to contemporaneous behaviors. Here is the line of reasoning:

“Limestone put on the soil lessens the acidity, and limestone put on the soil grows clover. Therefore the change in acidity must be the cause of the growing clover.”

At the same time, there was disregarded another possible deduction, namely:

“Limestone put on the soil applies the plant nutrient calcium. Therefore the applied calcium must be the cause of the growth of clover.”

The labeling of calcium as a fertilizer element of first importance was delayed because scientists, like other boys, enjoyed playing with their toys. The advent of electrical instruments for measuring the hydrogen ion concentration gave tools and inducement to measure soil acidity everywhere. The pH values were determined on slight provocations and causal significance was widely ascribed to them when, as a matter of fact, the degree of acidity, like temperature, is a condition and not a cause of many soil chemical reactions.

Because this blind alley of soil acidity was accepted as a thoroughfare for so long and because no simple instrument for measuring calcium ionization was available, it has taken extensive plant studies to demonstrate the hidden calcium hungers in plants responsible, in turn, for hidden but more extensive hungers in animals. Fortunately, a truce has recently been declared in the fight over soil acidity. What was once considered a malady is now considered a beneficial condition of the soil. Instead of a bane, soil acidity is a blessing in that many plant nutrients applied to such soil are made more serviceable by its presence, and soil acidity is an index of how seriously our attention must go to the declining soil fertility.

Now we face new concepts of the mechanisms of plant nutrition. By means of studies using only the colloidal—or finer—clay fraction of the soil, it was learned that this soil portion is really an acid. It is also highly buffered, or takes on hydrogen, calcium, magnesium, and any other cations in relatively large quantities, to put them out of solution and out of extensive ionic activities. It demonstrated that because of its insolubility, it can hide away many plant nutrients, so that pure water will not remove them yet salt solutions will exchange with them. This absorption and exchange activity of clay is the basic principle that serves in plant nutrition. This concept comes as a by-product of the studies of calcium in relation to soil acidity.

Imagine that a soil consists of some calcium-bearing minerals of silt size mixed with acid clays. The calcium-bearing mineral interacts with the hydrogen of the acid clay. The hydrogen goes to the mineral in exchange for the calcium going to the clay. Imagine further that the plant root enters into this clay-and-mineral mixture. It does so more readily because of the presence of the clay. It excretes carbon dioxide (and possibly other compounds) into this moist mixture to give carbonic acid, with its ionized hydrogen, to carry on between the root acid and the clay particle and the mineral. The hydrogen from the root exchanges with the calcium absorbed on the clay in close contact.

Thus, plant nutrition is a trading business between root and mineral, with the clay serving as the jobber, or the “go-between.” The clay takes the hydrogen offered by the root, trades it to the silt minerals for the calcium, and then passes the calcium to the root. Thus nutrients such as calcium and other positive ions pass from the minerals to the clay and to the root, while hydrogen, or acidity, is passing in the opposite direction, to weather out of the soil its nutrient mineral reserve and leave, finally, the acid clay mixed with unweatherable quartz sand. Acid soils are, then, merely the indication of nutrient depletion.


Calcium plays more than the role of moving itself into the plant. This element is serving, apparently, in the mechanism of moving other nutrients into the plant (and possibly excluding some nonnutrients). Careful studies of plants growing on colloidal clay have shown that no growth is possible unless calcium is moved into the crop. As the supply of calcium becomes lower, the crop may be growing, but it is losing back to the soil some of the potassium, some of the nitrogen, some of the phosphorus, and even some of the magnesium planted in the seed while taking none of these nutrients from the soil. Unless the calcium is serving its function in the plant, the crop may be growing and [yet] contain, in both the top and the root, less nitrogen, potassium, and phosphorus than was in the planted seed.

Here is an unappreciated service by calcium. For example, calcium is associated with an increased delivery of phosphorus to a crop: a phosphorus application on limed land puts three times as much phosphorus into a crop as when phosphate fertilizer is applied without lime. Calcium is also associated with more effective movement of nitrogen from the soil into a crop. And it plays some role, possibly in the mechanism of the root membrane through which phosphorus goes more efficiently perhaps as a calcium phosphate than as any other form. [sic] Nitrogen may go through more effectively as a nitrate. Here are some services by calcium of which the details of mechanism will be fully elucidated only by future researches.

Calcium plays what might be termed the leadership role among the nutrient ions, not only as to their entrance into the plants but also as to their combination into the proteinaceous compounds around which cell multiplication and life itself center. As the protein concentration of forages rises, there is an increase in the calcium concentration. Also, there is accumulation of evidence that with the increase in protein there goes an increase in vitamins. Legumes—the most nutritious of the forages—have long been known for their demand for calcium and high content of protein. They are also high in other minerals, so that calcium in the plants seems to synthesize the soilborne nutrients into the organic combinations though it does not itself appear as part of the final products.

Potassium, quite unlike calcium, is more directly effective in the compounding of air and water into carbohydrates, though, like calcium, it does not itself appear in them. Potassium is effective in making bulk, or tonnage, of forage. Calcium is effective in bringing higher concentration of proteins and other nutrients essential within that bulk. Accordingly, as the active calcium dominates the supplies of nutrients in the soil, proteinaceousness—and with it a high content of growth minerals—characterizes the vegetation produced on the soil. As potassium dominates, there is plenty of plant bulk, but its composition is highly carbonaceous, or it is dominantly woody.

Here is a general principle that is helpful in understanding the ecological array of vegetation. According to it, the vegetation is highly proteinaceous and mineral-rich on our prairies in the soil regions of lower rainfall or those soils retaining a high mineral content in which calcium is prominent. Contrariwise, vegetation is mainly wood—or like the forest—on the more leached soils, with lower mineral content but with potassium naturally dominant.

This ecological picture served as a stimulus for some soil studies of the chemical activities of potassium and calcium when present [in] clay in different ratios. Prof. C.E. Marshall of the University of Missouri has designed electrodes and membranes for measuring the ionic activity of calcium and potassium of the soil in the same way that hydrogen ion activities are measured. His data of what might be called pK and pCa—in the same manner as we speak of pH—demonstrate clearly that the ionic activities in a mixture of elements are not independent of each other, as is true in mixtures of gases. Rather, they are complimentary in some combinations and opposing in others. Considering calcium and potassium in combination, the latter gains ascendancy in relative activities as the ratio between the calcium and the potassium becomes narrower. Thus, the more calcium is weathered out of the soil, the more active potassium becomes in moving into the plant. Here is the physicochemical soil situation provoking the protein-carbohydrate relation, which in turn represents the “grow” foods versus “go” foods situation so prominently basic in our hidden hungers and disturbed animal nutrition.

The soil, because it is nourishment to make one kind of plant or another—that is, whether the plants are truly nourishment for animals or are only so much internal packing material—is the real basis for and real help in understanding animal distribution, whether wild or domestic, lower or higher. Cattle growing with ease and success is common in Texas but [the practice] meets increasing difficulties as one goes eastward. Donkeys are “sweethearts of the desert,” where their sure-footedness among rock soils—and sturdy but fine bones—may well be associated with highly calcareous feeds grown in more arid regions.

[When donkey are] crossbred with the horse, the resulting hybrid, or mule, is at home farther east, in higher rainfalls and on more-leached soil areas. But even then, he is found most commonly on the limestone soils of Missouri, Arkansas, Kentucky, and Tennessee. The mule grown to maturity in these areas and then shipped to the cottony South survives to render labor because, with no hope for posterity, the calcium supply transported within him, in his bones, is not depleted by reproductive demands.

Picture further the sheep and goat according to their concentration in different geographic areas. With them go the increase of so-called “troubles and bad luck” in raising them [when] they are in the humid, more-acid soil regions.

Soil fertility, so prominent as the foundation of animal reproductive performances, has not been appreciated [in this regard]. We need to see our most nutritious foods in those animal products connected with the reproduction of the animal—namely, eggs and milk. Reproduction goes forward only on a plane of liberal supplies of soil fertility and is therefore the safety factor in our living, and it can be a safety factor in our thinking.

This picture of animal ecology—and its nutritional reasons based on the soil—does not present itself without calcium playing a prominent part in the causal forces. Soil treatments that supply calcium in the humid regions are readily detected by the animal when it is given an opportunity to manifest a choice of grazing on herbages in differently treated areas.

Domestication has dulled the instinct for wise food choice in some animals. For example, greediness of the high-producing milk cow brings bloat on herself. (This is less common among cows not so highly domesticated toward intensive milk production.) Nevertheless, there is still enough appetite instinct left in the cow that she refuses to eat the grass where urine was dropped, [which] brings about unbalanced plant composition by an excessive nitrogen application.

Her refusal to eat sweet clover and her preference for bluegrass over white clover are evidence that this foster mother of the human race is her own nutritionist and knows her carbohydrate-protein ratios for a well-balanced diet. She is demonstrating daily her appreciation of the whole series of effects and causes in variable plant composition as they go back through vegetation to the soil [and] demonstrate relations between calcium and potassium and other nutrient ions of the soil. We need to observe our animals and learn from them. When we accuse the mule of stubbornness in his refusal to eat or to drink, the reflection may not be on this dumb beast as much as on his master, too stubborn to learn from nature.


By means of the biological assay, our animals are telling us that they can be fed more efficiently by wise fertilizer treatments of the soil. Soil treatment is not merely a case of [aiding] plants’ service as mineral haulers, to carry calcium from the field to the animal feedbag; rather, for example, lime is applied to make the plant factory more efficient in gathering its various nutrients from the soil and still more efficient in synthesizing these with carbon, hydrogen, and oxygen from air and water into the extensive list of complexes and compounds whose service to growth and good health we are slowly unraveling. Soil management is more than a practice guided by economics; it is a responsibility of nourishing microbes, plants, animals, and humans to their best growth and health.

Animal-growth studies testify to the importance of liming for its help in better animal nutrition. Sheep studies and rabbit feeding trials using Missouri soils with various forages point clearly to the more efficient conversion of roughages into meat when lime is used as a soil treatment. Increases in animal growth as high as 50 percent from the same amount of feed consumed are efficiencies that surely cannot be disregarded when food is to win the war and protein is the particular food deficiency. In terms of production with reduced labor, the better feeding of animals by means of soil treatments surely must not be neglected when the same acre with a constant labor input can deliver so much more as food products, in the form of meat.

Improved products from animals come in for greater efficiency also by way of lime and fertilizer used on the soil. The wool of sheep fed hay grown on soil given lime and phosphate was improved [versus that of sheep fed hay] grown where only phosphate was used. Fatty secretions were visibly different, but quality differences in the fiber were revealed upon scouring the wool. Another animal secretion, milk—so commonly considered of constant nutrient value—has permitted rickets in calfs [grazing] on soils deficient in lime, irrespective of ample green feed and ample sunshine for both mother and calf.

Animals and their products have [always] been a safety factor in man’s diet—in that animals are additional aid in collecting, from a wider range, all possible helps toward the food man needs. Historic man’s survival has possibly been more largely the result of his herds and flocks than we are wont to believe. But even with the help of animals, the soils may still be so deficient that animal products fail to give the full service commonly credited to them. As we push meat and animal products out of their more common place in our diet, and as we go more nearly to strictly vegetarianism, the attention to the soil is all the more important.

Man scarcely dares circumvent the animal in the biotic pyramid suggested by Aldo Leopold, which includes soil, microbes, plants, animals, and man, in that order from the bottom upward. He may claim vegetarianism in that he survives without consuming meat, but seldom does he exclude milk, cheese, and fish completely and become strictly vegetarian. It is true that [people in] highly vegetarian nations such as China and Japan consume mainly rice. But though they are highly vegetarian, they are not so to the exclusion of a minimum of some chicken broth or fish. This fish, required for survival, may be merely the head of the animal, as reported by J.B. Powell, a journalist of Japanese prison experience, whose refusal to eat even this amount of animal product cost him his feet—lost by gangrene—when his companion prisoners, as fish-head eaters, were not so unfortunate.

Current attention to calcium and other fertility elements in the soil promises better nutrition and health. Although proper nutritional requirements are still very much the result of chemico-analytical thinking, we are yet discovering more essential parts in the proper diet. We are not yet strictly synthesizing purely chemical diets. A significant share of a good diet still consists of the so-called “natural” food, so that nature is still, for many of us, the best dietician, as we prefer to stake our future health on omnivorousness and plenty of natural foods from fertile soils. Synthetic diets will meet the supreme test not when they are merely able to make animals grow or keep them alive but, rather, when they can carry animals through their regular reproductive cycles for several generations, with numerous and healthy offspring.

The natural growth processes—initiated and guided in the main by the chemical nutrients coming from the soil—are still the main basis of nutrition. Calcium, as the foremost element on the list of the nutrients demanded from the soil, has given us a pattern of the importance of its role in nutrition. It points with suggestions of importance to the other nine or more elements whose nutritional significance we do not yet understand as well. Observations and scientific studies, under the present appreciation of our soil as the basis of health, will soon increase our knowledge of nutrition, as we recognize the larger principles as they apply to all the life forms, including microbes, plants, and animals no less than man. We shall rapidly come to recognize that our national health lies in our soil, and our future security lies in soil conservation guided by nutrition’s universal laws.

By William A. Albrecht, University of Missouri College of Agriculture, Columbia, Missouri. Reprinted with the author’s permission from The Land, Vol. 3, No. 1, December 1943, by the Lee Foundation for Nutritional Research. 

Reprint No. 8
Lee Foundation for Nutritional Research
Milwaukee 1, Wisconsin

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Note: Lee Foundation for Nutritional Research is a nonprofit, public service institution, chartered to investigate and disseminate nutritional information. The attached publication is not literature or labeling forany product, nor shall it be employed as such by anyone. In accordance with the right of freedom of the press guaranteed to the Foundation by the First Amendment of the U.S. Constitution, the attached publication is issued and distributed for informational purposes.


Patrick Earvolino, CN

Patrick Earvolino is a Certified Nutritionist and Special Projects Editor for Selene River Press, Inc.

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