Albrecht would probably have approved of the following chart that expresses the essential qualities of dryland and humid soils.

Soil Mineral Content by Climate Area

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.

Average Nutritional Content by 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