CHAPTER XIV.

Absorption by Soils of Solids from Solutions. Absorption of Gases, Air of Soils, [267].—Absorption of Solids, [267].—Desalination, [267].—Decolorization, [267].—Complexity of Soil-Action, Physical and Chemical, [268].—“Purifying” Action of Soils on Gases and Liquids, [269].—Waste of Fertilizers, [269].—Variation of Absorptive Power, [270].—Generalities Regarding Chemical Action and Exchange, [270].—Drain Waters, [271].—Distinctions not Absolute, [272].—Absorption or Condensation of Gases by the Soil, [272].—Proof of Presence of Carbonic and Ammonia Gases in Soils, [273].—Absorption of Gases by Dry Soils. Figure, [274].—Composition of Gases Absorbed by Various Bodies from the Air. Table, [275].—Discussion of Table, [277].—The Air of Soils, [279].—Empty Space in Dry Soils, [279].—Functions of Air in Soils, [279].—Insufficient and Excessive Aeration, [280].—Composition of the Free Air of Soils, [280].—Carbonic Dioxid vs. Oxygen, [281].—Relation to Bacterial and Fungous Activity, [281].—Putrefactive Processes, [282].

CHAPTER XV.

Colors of Soils, [283].—Black Soils, [283].—“Red” Soils, [284].—Origin of Red Tints, [285].—White Soils, [285].—Differences in Arid and Humid Regions, [286].—White Alkali Spots, [286].

CHAPTER XVI.

Climate, [287].—Heat and Moisture Control Climates, [287].—Climatic Conditions, [287].—Ascertainment and Presentation of Temperature Conditions, [288].—Annual Mean not a Good Criterion, [289].—Extremes of Temperature are most Important, [289].—Seasonal and Monthly Means, [289].—Daily Variations, [290].—The Rainfall, [290].—Annual Rainfall not a Good Criterion, [290].—Distribution most Important, [290].—Winds, [291].—Heat the Cause of Winds, [291].—Trade Winds, [291].—Cyclones, [292].— Influence of the Topography on Winds; Rains to Windward of Mountains, Arid Climates to Leeward, [293].—General Distribution of Rainfall on the Globe. Figure, [294].—Ocean Currents, [295].—The Gulf Stream, [295].—The Japan Stream, [296].—Contrast of Climates of N. W. America, [297].—Continental, Coast and Insular Climates, [297].—Subtropic. Arid Belts, [298].—Utilization of the Arid Belts, [299].

CHAPTER XVII.

Relations of Soils and Plant Growth to Heat, [301].—Temperature of Soils, [301].—Water Exerts Controlling Influence, [301].—Cold and Warm Rains, [302].—Solar Radiation, [302].—Penetration of the Sun’s Heat into the Soil, [302].—Change of Temperature with Depth, [303].—Surface Conditions that Influence Soil Temperature, [303].—Heat of High and Low Intensity, [304].—Reflection vs. Dispersion of Heat, [304].—Influence of Vegetation, and of Mulches, [305].—Influence of the Nature of the Soil-Material, [306].—Influence of Evaporation, [307].—Formation of Dew, [307].—Dew rarely adds Moisture, [308].—Dew within the Soil, [308].—Plant Development under Different Temperature-Conditions, [309].—Germination of Seeds; Optimum Temperature for each Kind, [309].—Artificial Heating of Soils; by Steam Pipes or Water, [310].

CHAPTER XVIII.

Physico-chemical Investigation of Soils in Relation to Crop Production, [313].—Historical Review of Soil Investigation, [313].—Popular Forecasts of Soil Values, [313].—Cogency of Conclusions Based upon Native Growth, [314].—Ecological Studies, [315].—Early Soil Surveys of Kentucky, Arkansas and Mississippi, [316].—Investigation of Cultivated Soils, [316].—Change of Views, [317].—Advantages for Soil Study offered by Virgin Lands, [318].—Practical Utility of Soil Analysis; Permanent Value vs. Immediate Productiveness, [319].—Physical and Chemical Conditions of Plant Growth, [319].—Condition of Plant-food Ingredients, in the Soil, [319].—Water-soluble, Reserve, and Insoluble Part, [320].—Hydrous or “Zeolitic” Silicates, [321].—Recognition of the Prominent Chemical Character of Soils, [322].—Acidity, Neutrality and Alkalinity, [322].—Chemical Analysis, [323].—Water-Soluble and Acid-Soluble Portions most Important, [324].—We cannot Imitate Plant-root Action, 324 Cultural Experience the Final Test, [324].—Analysis of Cultivated Soils, [325].—Methods of Analysis, [325].—The Solvent Action of Water upon Soils, [327].—Extraction of Soils with Pure Water, [327].—Continuous Solubility of Soil Ingredients. Tables, [328].—King’s Results. Table, [329].—Composition and Analysis of Janesville Loam, [331].—Solubility of Soil Phosphates in Water, [332].—Practical Conclusions from Water Extraction, [332].—Ascertainment of the Immediate Plant-food Requirements of Cultivated Soils by Physiological Tests, [333].—Plot Tests; their uncertainties. Diagram, [334].—Crop Analysis as a Test of Soil Character, [337].—Chemical Tests of immediately Available Plant Food; Dyer’s Method, [338].