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"Within regions of similar moisture conditions, the organic matter content of soil . . . decreases from north to south. For each fall of 10° C (18° F) in annual temperature the average organic matter content of soil increases two or three times, provided that [soil moisture] is kept constant."
Moist soil during the growing season encourages plant
growth and thus organic matter production. Where the soil becomes dry during the
growing season, plant growth slows or stops. So, all things being equal, wet soils
contain more organic matter than dry ones. All organic matter eventually rots, even
in soil too dry to grow plants. The higher the soil temperature the faster the decomposition.
But chilly (not frozen) soils can still grow a lot of biomass. So, all things being
equal, hot soils have less humus in them than cold ones. Cool, wet soils will have
the highest levels; hot, dry soils will be lowest in humus.
This model checks out in practice. If we were to measure
organic matter in soils along the Mississippi River where soil moisture conditions
remain pretty similar from south to north, we might find 2 percent in sultry Arkansas,
3 percent in Missouri and over 4 percent in Wisconsin, where soil temperatures are
much lower. In Arizona, unirrigated desert soils have virtually no organic matter.
In central and southern California where skimpy and undependable winter rains peter
out by March, it is hard to find an unirrigated soil containing as much as 1 percent
organic matter while in the cool Maritime northwest, reliable winter rains keep the
soil damp into June and the more fertile farm pastures or natural prairies may develop
as much as 5 percent organic matter.
Other factors, like the basic mineral content of the soil
or its texture, also influence the amount of organic matter a spot will create and
will somewhat increase or decrease the humus content compared to neighboring locations
experiencing the same climate. But the most powerfully controlling influences are
moisture and temperature.
On all virgin soils the organic matter content naturally
sustains itself at the highest possible level. And, average annual additions exactly
match the average annual amount of decomposition. Think about that for a moment.
Imagine that we start out with a plot of finely-ground rock particles containing
no life and no organic matter. As the rock dust is colonized by life forms that gradually
build in numbers it becomes soil. The organic matter created there increases nutrient
availability and accelerates the breakdown of rock particles, further increasing
the creation of organic matter. Soil humus steadily increases. Eventually a climax
is sustained where there is as much humus in the soil as there can be.
The peak plant and soil ecology that naturally lives on any
site is usually very healthy and is inevitably just as abundant as there is moisture
and soil minerals to support it. To me this suggests how much organic matter it takes
to grow a great vegetable garden. My theory is that in terms of soil organic matter,
vegetables grow quite well at the humus level that would peak naturally on a virgin
site. In semi-arid areas I'd modify the theory to include an increase as a result
of necessary irrigation. Expressed as a rough rule of thumb, a mere 2 percent organic
matter in hot climates increasing to 5 percent in cool ones will supply sufficient
biological soil activities to grow healthy vegetables if the mineral nutrient
levels are high enough too.
Recall my assertion that what is most important about organic
matter is not how much is present, but how much is lost each year through decomposition.
For only by decomposing does organic matter release the nutrients it contains so
plants can uptake them; only by being consumed does humus support the microecology
that so markedly contributes phytamins to plant nutrition, aggressively breaks down
rock particles and releases the plant nutrients they contain; only by being eaten
does soil organic matter support bacteria and earthworms that improve productivity
and create better tilth.
Here's something I find very interesting. Temperate climates
having seasons and winter, vary greatly in average temperature. Comparing annual
decomposition loss from a hot soil carrying 2 percent humus with annual decomposition
loss from a cooler soil carrying 5 percent, roughly the same amount of organic matter
will decay out of each soil during the growing season. This means that in temperate
regions we have to replace about the same amount of organic matter no matter what
the location.
Like other substantial colleges of agriculture, the University
of Missouri ran some very valuable long-term studies in soil management. In 1888,
a never-farmed field of native prairie grasses was converted into test plots. For
fifty succeeding years each plot was managed in a different but consistent manner.
The series of experiments that I find the most helpful recorded what happens to soil
organic matter as a consequence of farming practices. The virgin prairie had sustained
an organic matter content of about 3.5 percent. The lines on the graph show what
happened to that organic matter over time.

Timothy grass is probably a slightly more efficient converter
of solar energy into organic matter than was the original prairie. After fifty years
of feeding the hay cut from the field and returning all of the livestock's manure,
the organic matter in the soil increased about 1/2 percent. Obviously, green manuring
has very limited ability to increase soil humus above climax levels. Growing oats
and returning enough manure to represent the straw and grain fed to livestock, the
field held its organic matter relatively constant.
Growing small grain and removing everything but the stubble
for fifty years greatly reduced the organic matter. Keep in mind that half the biomass
production in a field happens below ground as roots. And keep in mind that the charts
don't reveal the sad appearance the crops probably had once the organic matter declined
significantly. Nor do they show that the seed produced on those degenerated fields
probably would no longer sprout well enough to be used as seedgrain, so new seed
would have been imported into the system each season, bringing with it new supplies
of plant nutrients. Without importing that bushel or so of wheat seed on each acre
each year, the curves would have been steeper and gone even lower.
Corn is the hardest of the cereals on soil humus. The reason
is, wheat is closely broadcast in fall and makes a thick grassy overwintering stand
that forms biomass out of most of the solar energy striking the field from spring
until early summer when the seed forms. Leafy oats create a little more biomass than
wheat. Corn, on the other hand, is frost tender and can't be planted early. It is
also not closely planted but is sown in widely-spaced rows. Corn takes quite a while
before it forms a leaf canopy that uses all available solar energy. In farming lingo,
corn is a "row crop."
Vegetables are also row crops. Many types don't form dense
canopies that soak up all solar energy for the entire growing season like a virgin
prairie. As with corn, the ground is tilled bare, so for much of the best part of
the growing season little or no organic matter is produced. Of all the crops that
a person can grow, vegetables are the hardest on soil organic matter. There is no
way that vegetables can maintain soil humus, even if all their residues are religiously
composted and returned. Soil organic matter would decline markedly even in an experiment
in which we raised some small animals exclusively on the vegetables and returned
all of their manure and urine too.
When growing vegetables we have to restore organic matter
beyond the amount the garden itself produces. The curves showing humus decline at
the University of Missouri give us a good hint as to how much organic matter we are
going to lose from vegetable gardening. Let's make the most pessimistic possible
estimate and suppose that vegetable gardening is twice as hard on soil as was growing
corn and removing everything but the stubble and root systems.
With corn, about 40 percent of the entire organic matter
reserve is depleted in the first ten years. Let's suppose that vegetables might remove
almost all soil humus in ten years, or 10 percent each year for the first
few years. This number is a crude. and for most places in America, a wildly pessimistic
guess.
However, 10 percent loss per year may understate losses in
some places. I have seen old row crop soils in California's central valley that look
like white-colored blowing dust. Nor does a 10 percent per year estimate quite allow
for the surprising durability I observe in the still black and rich-looking old vegetable
seed fields of western Washington State's Skaget Valley. These cool-climate fields
have suffered chemical farming for decades without having been completely destroyed--yet.
How much loss is 10 percent per year? Let's take my own garden
for example. It started out as an old hay pasture that hadn't seen a plow for twenty-five
or more years and where, for the five years I've owned the property, the annual grass
production is not cut, baled, and sold but is cut and allowed to lie in place. Each
year's accumulation of minerals and humus contributes to the better growth of the
next year's grass. Initially, my grass had grown a little higher and a little thicker
each year. But the steady increase in biomass production seems to have tapered off
in the last couple of years. I suppose by now the soil's organic matter content probably
has been restored and is about 5 percent.
I allocate about one acre of that old pasture to garden land.
In any given year my shifting gardens occupy one-third of that acre. The other two-thirds
are being regenerated in healing grass. I measure my garden in fractions of acres.
Most city folks have little concept of an acre; its about 40,000 square feet, or
a plot 200' x 200'.
Give or take some, the plow pan of an acre weighs about two
million pounds. The plow pan is that seven inches of topsoil that is flipped over
by a moldboard plow, the seven inches where most biological activity occurs, where
virtually all of the soil's organic matter resides. Two million pounds equals one
thousand tons of topsoil in the first seven inches of an acre. Five percent of that
one thousand tons can be organic matter, up to fifty priceless tons of life that
changes 950 tons of dead dust into a fertile, productive acre. If 10 percent of that
fifty tons is lost as a consequence of one year's vegetable gardening, that amounts
to five tons per acre per year lost or about 25 pounds lost per 100 square feet.
Patience, reader. There is a very blunt and soon to be a
very obvious point to all of this arithmetic. Visualize this! Lime is spread at rates
up to four tons per acre. Have you ever spread 1 T/A or 50 pounds of lime over a
garden 33 x 33 feet? Mighty hard to accomplish! Even 200 pounds of lime would barely
whiten the ground of a 1,000 square-foot garden. It is even harder to spread a mere
5 tons of compost over an acre or only 25 pounds on a 100-square-foot bed. It seems
as though nothing has been accomplished, most of the soil still shows, there is no
layer of compost, only a thin scattering.
But for the purpose of maintaining humus content of vegetable
ground at a healthy level, a thin scattering once a year is a gracious plenty. Even
if I were starting with a totally depleted, dusty, absolutely humusless, ruined old
farm field that had no organic matter whatsoever and I wanted to convert it to a
healthy vegetable garden, I would only have to make a one-time amendment of 50 tons
of ripe compost per acre or 2,500 pounds per 1,000 square feet. Now 2,500 pounds
of humus is a groaning, spring-sagging, long-bed pickup load of compost heaped up
above the cab and dripping off the sides. Spread on a small garden, that's enough
to feel a sense of accomplishment about. Before I knew better I used to incorporate
that much composted horse manure once or twice a year and when I did add a half-inch
thick layer that's about what I was applying.
Fertilizing Vegetables with Compost
Will a five ton per acre addition of compost provide enough
nutrition to grow great vegetables? Unfortunately, the answer usually is no. In most
gardens, in most climates, with most of what passes for "compost," it probably
won't. That much compost might well grow decent wheat.
The factors involved in making this statement are numerous
and too complex to fully analyze in a little book like this one. They include the
intrinsic mineralization of the soil itself, the temperature of the soil during the
growing season, and the high nutritional needs of the vegetables themselves. In my
experience, a few alluvial soils that get regular, small additions of organic matter
can grow good vegetable crops without additional help. However, these sites are regularly
flooded and replenished with highly mineralized rock particles. Additionally, they
must become very warm during the growing season. But not all rock particles contain
high levels of plant nutrients and not all soils get hot enough to rapidly break
down soil particles.
Soil temperature has a great deal to do with how effectively
compost can act as fertilizer. Sandy soils warm up much faster in spring and sand
allows for a much freer movement of air, so humus decomposes much more rapidly in
sand. Perhaps a sunny, sandy garden on a south-facing slope might grow pretty well
with small amounts of strong compost. As a practical matter, if most people spread
even the most potent compost over their gardens at only twenty-five pounds per 100
square feet, they would almost certainly be disappointed.
Well then, if five tons of quality compost to the acre isn't
adequate for most vegetables, what about using ten or twenty tons of the best. Will
that grow a good garden? Again, the answer must allow for a lot of factors but is
generally more positive. If the compost has a low C/N and that compost, or the soil
itself, isn't grossly deficient in some essential nutrient, and if the soil has a
coarse, airy texture that promotes decomposition, then somewhat heavier applications
will grow a good-looking garden that yields a lot of food.
However, one question that is rarely asked and even more
rarely answered satisfactorily in the holistic farming and gardening lore is: Precisely
how much organic matter or humus is needed to maximize plant health and the nutritional
qualities of the food we're growing? An almost equally important corollary of this
is: Can there be too much organic matter?
This second question is not of practical consequence for
biological grain/livestock farmers because it is almost financially impossible to
raise organic matter levels on farm soils to extraordinary amounts. Large-scale holistic
farmers must grow their own humus on their own farm. Their focus cannot be on buying
and bringing in large quantities of organic matter; it must be on conserving and
maximizing the value of the organic matter they produce themselves.
Where you do hear of an organic farmer (not vegetable grower
but cereal/livestock farmer) building extraordinary fertility by spreading large
quantities of compost, remember that this farmer must be located near an inexpensive
source of quality material. If all the farmers wanted to do the same there would
not be enough to go around at an economic price unless, perhaps, the entire country
became a "closed system" like China. We would have to compost every bit
of human excrement and organic matter and there still wouldn't be enough to meet
the demand. Even if we became as efficient as China, keep in mind the degraded state
of China's upland soils and the rapid desertification going on in their semi-arid
west. China is robbing Peter to pay Paul and may not have a truly sustainable agriculture
either.
I've frequently encountered a view among devotees of the
organic gardening movement that if a little organic matter is a good thing, then
more must be better and even more better still. In Organic Gardening magazine and
Rodale garden books we read eulogies to soils that are so high in humus and so laced
with earthworms that one can easily shove their arm into the soft earth elbow deep
but must yank it out fast before all the hairs have been chewed off by worms, where
one must jump away after planting corn seeds lest the stalk poke you in the eye,
where the pumpkins average over 100 pounds each, where a single trellised tomato
vine covers the entire south side of a house and yields bushels. All due to compost.
I call believers of the organic faith capital "O"
organic gardeners. These folks almost inevitably have a pickup truck used to gather
in their neighborhood's leaves and grass clippings on trash day and to haul home
loads from local stables and chicken ranches. Their large yards are ringed with compost
bins and their annual spreadings of compost are measured in multiples of inches.
I was one once, myself.
There are two vital and slightly disrespectful questions
that should be asked about this extreme of gardening practice. Is this much humus
the only way to grow big, high-yielding organic vegetable gardens and two, are vegetables
raised on soils super-high in humus maximally nutritious. If the answer to the first
question is no, then a person might avoid a lot of work by raising the nutrient level
of their soil in some other manner acceptable to the organic gardener. If the answer
to the second question is less nutritious, then serious gardeners and homesteaders
who are making home-grown produce into a significant portion of their annual caloric
intake had better reconsider their health assumptions. A lot of organic gardeners
cherish ideas similar to the character Woody Allen played in his movie, Sleeper.
Do you recall that movie? It is about a contemporary American
who, coming unexpectedly close to death, is frozen and then reanimated and healed
200 years in the future. However, our hero did not expect to die or be frozen when
he became ill and upon awakening believes the explanation given to him is a put on
and that his friends are conspiring to make him into a fool. The irritated doctor
in charge tells Woody to snap out of it and be prepared to start a new life. This
is no joke, says the doctor, all of Woody's friends are long since dead. Woody's
response is a classic line that earns me a few chuckles from the audience every time
I lecture: 'all my friends can't be dead! I owned a health food store and we all
ate brown rice.'
Humus and the Nutritional Quality of Food
I believe that the purpose of food is not merely to fill
the belly or to provide energy, but to create and maintain health. Ultimately, soil
fertility should be evaluated not by humus content, nor microbial populations, nor
earthworm numbers, but by the long-term health consequences of eating the food. If
physical health degenerates, is maintained, or is improved we have measured the soil's
true worth. The technical name for this idea is a "biological assay." Evaluating
soil fertility by biological assay is a very radical step, for connecting long-term
changes in health with the nutritional content of food and then with soil management
practices invalidates a central tenet of industrial farming: that bulk yield is the
ultimate measure of success or failure. As Newman Turner, an English dairy farmer
and disciple of Sir Albert Howard, put it:
"The orthodox scientist normally measures the fertility of a soil by its bulk yield, with no relation to effect on the ultimate consumer.
I have seen cattle slowly lose condition and fall in milk yield when fed entirely on the abundant produce of an apparently fertile soil. Though the soil was capable of yielding heavy crops, those crops were not adequate in themselves to maintain body weight and milk production in the cow, without supplements. That soil, though capable of above-average yields, and by the orthodox quantitative measure regarded as fertile, could not, by the more complete measure of ultimate effect on the consumer, be regarded but anything but deficient in fertility.
Fertility therefore, is the ability to produce at the highest recognized level of yield, crops of quality which, when consumed over long periods by animals or man, enable them to sustain health, bodily condition and high level of production without evidence of disease or deficiency of any kind.
Fertility cannot be measured quantitatively. Any measure of soil fertility must be related to the quality of its produce. . . . the most simple measure of soil fertility is its ability to transmit, through its produce, fertility to the ultimate consumer."
Howard also tells of creating a super-healthy herd of
work oxen on his research farm at Indore, India. After a few years of meticulous
composting and restoration of soil life, Howard's oxen glowed with well-being. As
a demonstration he intentionally allowed his animals to rub noses across the fence
with neighboring oxen known to be infected with hoof and mouth and other cattle plagues.
His animals remained healthy. I have read so many similar accounts in the literature
of the organic farming movement that in my mind there is no denying the relationship
between the nutritional quality of plants and the presence of organic matter in soil.
Many other organic gardeners reach the same conclusion. But most gardeners do not
understand one critical difference between farming and gardening: most agricultural
radicals start farming on run-down land grossly deficient in organic matter. The
plant and animal health improvements they describe come from restoration of soil
balance, from approaching a climax humus level much like I've done in my pasture
by no longer removing the grass.
But home gardeners and market gardeners near cities are able
to get their hands on virtually unlimited quantities of organic matter. Encouraged
by a mistaken belief that the more organic matter the healthier, they enrich their
soil far beyond any natural capacity. Often this is called "building up the
soil." But increasing organic matter in gardens well above a climax ecology
level does not further increase the nutritional value of vegetables and in many circumstances
will decrease their value markedly.
For many years I have lectured on organic gardening to the
Extension Service's master gardener classes. Part of the master gardener training
includes interpreting soil test results. In the early 1980s when Oregon State government
had more money, all master gardener trainees were given a free soil test of their
own garden. Inevitably, an older gentlemen would come up after my lecture and ask
my interpretation of his puzzling soil test.
Ladies, please excuse me. Lecturing in this era of women's
lib I've broken my politically incorrect habit of saying "the gardener, he .
. ." but in this case it was always a man, an organic gardener who had
been building up his soil for years.
The average soils in our region test moderately- to strongly
acid; are low in nitrogen, phosphorus, calcium, and magnesium; quite adequate in
potassium; and have 3-4 percent organic matter. Mr. Organic's soil test showed an
organic matter content of 15 to 20 percent with more than adequate nitrogen and a
pH of 7.2. However there was virtually no phosphorus, calcium or magnesium and four
times the amount of potassium that any farm agent would ever recommend. On the bottom
of the test, always written in red ink, underlined, with three exclamation points,
"No more wood ashes for five years!!!" Because so many people in the Maritime
northwest heat with firewood, the soil tester had mistakenly assumed that the soil
became alkaline and developed such a potassium imbalance from heavy applications
of wood ashes.
This puzzled gardener couldn't grasp two things about his
soil test report. One, he did not use wood ashes and had no wood stove and two, although
he had been "building up his soil for six or seven years," the garden did
not grow as well as he had imagined it would. Perhaps you see why this questioner
was always a man. Mr. Organic owned a pickup and loved to haul organic matter and
to make and spread compost. His soil was full of worms and had a remarkably high
humus level but still did not grow great crops.
It was actually worse than he understood. Plants uptake as
much potassium as there is available in the soil, and concentrate that potassium
in their top growth. So when vegetation is hauled in and composted or when animal
manure is imported, large quantities of potassium come along with them. As will be
explained shortly, vegetation from forested regions like western Oregon is even more
potassium-rich and contains less of other vital nutrients than vegetation from other
areas. By covering his soil several inches thick with manure and compost every year
he had totally saturated the earth with potassium. Its cation exchange capacity or
in non-technical language, the soil's ability to hold other nutrients had been overwhelmed
with potassium and all phosphorus, calcium, magnesium, and other nutrients had largely
been washed away by rain. It was even worse than that! The nutritional quality of
the vegetables grown on that superhumusy soil was very, very low and would have been
far higher had he used tiny amounts of compost and, horror of all horrors, chemical
fertilizer.
Climate and the Nutritional Quality of Food
Over geologic time spans, water passing through soil leaches
or removes plant nutrients. In climates where there is barely enough rain to grow
cereal crops, soils retain their minerals and the food produced there tends to be
highly nutritious. In verdant, rainy climates the soil is leached of plant nutrients
and the food grown there is much less nutritious. That's why the great healthy herds
of animals were found on scrubby, semi-arid grasslands like the American prairies;
in comparison, lush forests carry far lower quantities of animal biomass.
Some plant nutrients are much more easily leached out than
others. The first valuable mineral to go is calcium. Semi-arid soils usually still
retain large quantities of calcium. The nutrient most resistant to leaching is potassium.
Leached out forest soils usually still retain relatively large amounts of potassium.
William Albrecht observed this data and connected with it a number of fairly obvious
and vital changes in plant nutritional qualities that are caused by these differences
in soil fertility. However obvious they may be, Albrecht's work was not considered
politically correct by his peers or the interest groups that supported agricultural
research during the mid-twentieth century and his contributions have been largely
ignored. Worse, his ideas did not quite fit with the ideological preconceptions of
J.l. Rodale, so organic gardeners and farmers are also ignorant of Albrecht's wisdom.
Albrecht would probably have approved of the following chart
that expresses the essential qualities of dryland and humid soils.
| Plant Nutrient | Dryland Prairie Soil | Humid Forest Soil |
| nitrogen | high | low |
| phosphorus | high | low |
| potassium | high | moderately high |
| calcium | very high | low |
| pH | neutral | acid |
Dryland soils contain far higher levels of all minerals than
leached soils. But Albrecht speculated that the key difference between these soils
is the ratio of calcium to potassium. In dryland soils there is much more
calcium in the soil than there is potassium while in wetter soils there is as much
or more potassium than calcium. To test his theory he grew some soybeans in pots.
One pot had soil with a high amount of calcium relative to the amount of potassium,
imitating dryland prairie soil. The other pot had just as much calcium but had more
potassium, giving it a ratio similar to a high quality farm soil in the eastern United
States. Both soils grew good-looking samples of soybean plants, but when they were
analyzed for nutritional content they proved to be quite different.
| Soil | Yield | Calories | Protein | Calcium | Phosphorus | Potassium |
| Humid | 17.8 gm | High | 13% | 0.27% | 0.14% | 2.15% |
| Dryland | 14.7 gm | Medium | 17% | 0.74% | 0.25% | 1.01% |
The potassium-fortified soil gave a 25 percent higher bulk
yield but the soybeans contained 25 percent less protein. The consumer of those plants
would have to burn off approximately 30 percent more carbohydrates to obtain the
same amount of vital amino acids essential to all bodily functions. Wet-soil plants
also contain only one-third as much calcium, an essential nutrient, whose lack over
several generations causes gradual reduction of skeletal size and dental deterioration.
They also contain only half as much phosphorus, another essential nutrient. Their
oversupply of potassium is not needed; humans eating balanced diets usually excrete
large quantities of unnecessary potassium in their urine.
Albrecht then analyzed dozens of samples of vegetation that
came from both dryland soils and humid soils and noticed differences in them similar
to the soybeans grown under controlled conditions. The next chart, showing the average
composition of plant vegetation from the two different regions, is taken directly
from Albrecht's research. The figures are averages of large numbers of plant samples,
including many different food crops from each climate.
| Nutrient | Dryland Soil | Humid Soil |
| Potassium | 2.44% | 1.27% |
| Calcium | 1.92% | 0.28% |
| Phosphorus | 0.78% | 0.42% |
| Total mineral nutrition | 5.14% | 1.97% |
| Ratio of Potassium to Calciuim | 1.20/1 | 4.50/1 |
Analyzed as a whole, these data tell us a great deal about
how we should manage our soil to produce the most nutritious food and about the judicious
use of compost in the garden as well. I ask you to refer back to these three small
charts as I point out a number of conclusions that can be drawn from them.
The basic nutritional problem that all animals have is not
about finding energy food, but how to intake enough vitamins, minerals and usable
proteins. What limits our ability to intake nutrients is the amount of bulk we can
process--or the number of calories in the food. With cows, for example, bulk is the
limiter. The cow will completely fill her digestive tract at all times and will process
all the vegetation she can digest every day of her life. Her health depends on the
amount of nutrition in that bulk. With humans, our modern lifestyle limits most of
us to consuming 1,500 to 1,800 calories a day. Our health depends on the amount of
nutrients coming along with those calories.
So I write the fundamental equation for human health as follows:
HEALTH = NUTRITION IN FOOD DIVIDED BY CALORIES IN THAT FOOD
If the food that we eat contains all of the nutrients that
food could possibly contain, and in the right ratios, then we will get sufficient
nutrition while consuming the calories we need to supply energy. However, to the
degree that our diet contains denatured food supplying too much energy, we will be
lacking nutrition and our bodies will suffer gradual degeneration. This is why foods
such as sugar and fat are less healthful because they are concentrated sources of
energy that contain little or no nutrition. Nutritionless food also contributes to
"hidden hungers" since the organism craves something that is missing. The
body overeats, and becomes fat and unhealthy.
Albrecht's charts show us that food from dry climates tends
to be high in proteins and essential minerals while simultaneously lower in calories.
Food from wet climates tends to be higher in calories while much lower in protein
and essential mineral nutrients. Albrecht's writings, as well as those of Weston
Price, and Sir Robert McCarrison listed in the bibliography, are full of examples
showing how human health and longevity are directly associated with these same variations
in climate, soil, and food nutrition.
Albrecht pointed out a clear example of soil fertility causing
health or sickness. In 1940, when America was preparing for World War II, all eligible
men were called in for a physical examination to determine fitness for military service.
At that time, Americans did not eat the same way we do now. Food was produced and
distributed locally. Bread was milled from local flour. Meat and milk came from local
farmers. Vegetables and potatoes did not all come from California. Regional differences
in soil fertility could be seen reflected in the health of people.
Albrecht's state, Missouri, is divided into a number of distinct
rainfall regions. The northwestern part is grassy prairie and receives much less
moisture than the humid, forested southeastern section. If soil tests were compared
across a diagonal line drawn from the northwest to the southeast, they would exactly
mimic the climate-caused mineral profile differences Albrecht had identified. Not
unexpectedly, 200 young men per 1,000 draftees were medically unfit for military
service from the northwest part of Missouri while 400 per 1,000 were unfit from the
southeastern part. And 300 per 1,000 were unfit from the center of the state.
Another interesting, and rather frightening, conclusion can
be drawn from the second chart. Please notice that by increasing the amount of potassium
in the potting soil, Albrecht increased the overall yield by 25 percent while simultaneously
lowering all of the other significant nutritional aspects. Most of this increase
of yield was in the form of carbohydrates, that in a food crops equates to calories.
Agronomists also know that adding potassium fertilizer greatly and inexpensively
increases yield. So American farm soils are routinely dosed with potassium fertilizer,
increasing bulk yield and profits without consideration for nutrition, or for the
ultimate costs in public health. Organic farmers often do not understand this aspect
of plant nutrition either and may use "organic" forms of potassium to increase
their yields and profits. Buying organically grown food is no guarantee that it contains
the ultimate in nutrition.
So, if health comes from paying attention to the ratio of
nutrition to calories in our food, then as gardeners who are in charge of creating
a significant amount of our own fodder, we can take that equation a step further:
| HEALTH | = | Nutrition/Calories | = | Calcium/Potassium |
When we decide how to manage our gardens we can take steps
to imitate dryland soils by keeping potassium levels lower while maintaining higher
levels of calcium.
Now take another close look at the third
chart. Average vegetation from dryland soils contains slightly more potassium
than calcium (1.2:1) while average vegetation from wetland soils contains many more
times more potassium than calcium (4.5:1). When we import manure or vegetation into
our garden or farm soils we are adding large quantities of potassium. Those of us
living in rainy climates that were naturally forested have it much worse in this
respect than those of us gardening on the prairies or growing irrigated gardens in
desert climates because the very vegetation and manure we use to "build up"
our gardens contains much more potassium while most of our soils already contain
all we need and then some.
It should be clear to you now why some organic gardeners
receive the soil tests like the man at my lecture. Even the soil tester, although
scientifically trained and university educated, did not appreciate the actual source
of the potassium overdose. The tester concluded it must have been wood ashes when
actually the potassium came from organic matter itself.
I conclude that organic matter is somewhat dangerous stuff
whose use should be limited to the amount needed to maintain basic soil tilth and
a healthy, complex soil ecology.
Fertilizing Gardens Organically
Scientists analyzing the connections between soil fertility
and the nutritional value of crops have repeatedly remarked that the best crops are
grown with compost and fertilizer. Not fertilizer alone and not compost alone. The
best place for gardeners to see these data is Werner Schupan's book (listed in the
bibliography).
But say the word "fertilizer" to an organic gardener
and you'll usually raise their hackles. Actually there is no direct linkage of the
words "fertilizer" and "chemical." A fertilizer is any concentrated
plant nutrient source that rapidly becomes available in the soil. In my opinion,
chemicals are the poorest fertilizers; organic fertilizers are far superior.
The very first fertilizer sold widely in the industrial world
was guano. It is the naturally sun-dried droppings of nesting sea birds that accumulates
in thick layers on rocky islands off the coast of South America. Guano is a potent
nutrient source similar to dried chicken manure, containing large quantities of nitrogen,
fair amounts of phosphorus, and smaller quantities of potassium. Guano is more potent
than any other manure because sea birds eat ocean fish, a very high protein and highly
mineralized food. Other potent organic fertilizers include seed meals; pure, dried
chicken manure; slaughterhouse wastes; dried kelp and other seaweeds; and fish meal.
| Material | % Nitrogen | % Phos. | % Potassium |
| Alfalfa meal | 2.5 | 0.5 | 2.1 |
| Bone meal (raw) | 3.5 | 21.0 | 0.2 |
| Bone meal (steamed) | 2.0 | 21.0 | 0.2 |
| Chicken manure (pure, fresh) | 2.6 | 1.25 | 0.75 |
| Cottonseed meal | 7.0 | 3.0 | 2.0 |
| Blood meal | 12.0 | 3.0 | -- |
| Fish meal | 8.0 | 7.0 | -- |
| Greensand | -- | 1.5 | 7.0 |
| Hoof and Horn | 12.5 | 2.0 | -- |
| Kelp meal | 1.5 | 0.75 | 4.9 |
| Peanut meal | 3.6 | 0.7 | 0.5 |
| Tankage | 11.0 | 5.0 | -- |
Growing most types of vegetables requires building a level
of soil fertility that is much higher than required by field crops like cereals,
soybeans, cotton and sunflowers. Field crops can be acceptably productive on ordinary
soils without fertilization. However, because we have managed our farm soils as depreciating
industrial assets rather than as relatively immortal living bodies, their ability
to deliver plant nutrients has declined and the average farmer usually must add additional
nutrients in the form of concentrated, rapidly-releasing fertilizers if they are
going to grow a profitable crop.
Vegetables are much more demanding than field crops. They
have long been adapted to growing on potent composts or strong manures like fresh
horse manure or chicken manure. Planted and nourished like wheat, most would refuse
to grow or if they did survive in a wheat field, vegetables would not produce the
succulent, tender parts we consider valuable.
Building higher than normal levels of plant nutrients can
be done with large additions of potent compost and manure. In semi-arid parts of
the country where vegetation holds a beneficial ratio of calcium to potassium food
grown that way will be quite nutritious. In areas of heavier rainfall, increasing
soil fertility to vegetable levels is accomplished better with fertilizers. The data
in the previous section gives strong reasons for many gardeners to limit the addition
of organic matter in soil to a level that maintains a healthy soil ecology and acceptable
tilth. Instead of supplementing compost with low quality chemical fertilizers, I
recommend making and using a complete organic fertilizer mix to increase mineral
fertility.
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