Mineral and Organic Components. Soil Organisms, Biology, and Nutrients. Homework III: The State Soil of Florida. Posted on website.

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Homework III: The State Soil of Florida Posted on website 5 bonus points Type all answers Soil Organisms, Biology, and Nutrients Mineral and Organic Components Functions of soils: recycler of raw materials Nutrient availability, replenishment 1

Organic Matter and Soil Biology Soil Organic Matter Accumulation of partially disintegrated and decomposed plant and animal residues plus biomass. 1 5% (by weight) in a typical, well-drained mineral soil Transitory soil constituent (hours to 100s of years) Requires continual addition to maintain O.M. levels. Constantly being broken down by soil micoorganisms Release/recycling of important plant nutrients Soil Organisms 2

What creatures live in soil? 22 species Harvester Ant Colony Fauna Macro Mammals, reptiles, amphibians, insects Micro Nematodes, Protozoa, Rotifers Flora 20,000 species Plant roots, algae, fungi, actinomycetes (filamentous bacteria), bacteria unicellular Basic Classification of Organisms Food Oxygen Demand Energy Source 3

Based on food: live or dead Herbivores Eat live plants Insects, mammals, reptiles Detritivores Eat dead tissues: Fungi, bacteria & actinomycetes Predators Eat other animals Insects, mammals, reptiles Based on O 2 demand Aerobic Active in O 2 rich environment Use free oxygen for metabolism Anaerobic Active in O 2 poor environment Use combined oxygen (NO - 3, SO -2 4 ) SO -2 4 => H 2 S Still Ponds O 2 NO 3 - SO 4-2 SO 4-2 H 2 S 4

Based on energy & C source Autotrophic (CO 2 ) Solar energy (photoautotrophs( photoautotrophs) Chemical reaction w/inorganic elements N, S, & Fe (chemoautotrophs( chemoautotrophs) Heterotrophic From breakdown of organic matter (Carbon) Most Numerous Quantification of Soil Organisms Quantification of Soil Organisms Numbers of organisms Extremely numerous 1,000,000-1,000,000,000 1,000,000,000 /g soil 10,000 species /g soil Biomass Three Criteria 1-8% of total soil organic matter Metabolic activity Respiration: CO 2 Proportional to # & biomass 5

Soil Organisms in Surface Soils Organisms #/g soil Biomass (g/m 2 ) Microflora Bacteria 10 8-10 40-500 Actinomycetes 10 7-10 40-500 Fungi 10 5-10 100-1,500 1,500 Algae 10 4-10 1-50 Fauna Protozoa 10 4-10 2-2020 Nematodes 10-10 1-1515 Mites 1-10 1-2 Earthworms 1-10 10-150 150 Note those in White Earthworms 1,000,000 per acre five pairs of hearts Mostly intestine 22 ft. long (Afr. and Aus.) Earthworm cast Casts: earthworm s s wastes Eat soil organics: 2-302 times of their own wt. Earthworms Abundance of earthworms 10-1,000/m 1,000/m 3 3,000 species Benefits of earthworms - soil fertility by producing cast (concentration of nutrients) - aeration & drainage - size & stability of soil aggregates 6

Autotrophs Soil Algae Capable of photosynthesis (chlorophyll) 1-1010 billion/ m 2 (can be mat of algae on surface) Prefer moist environments Rich in wetland and paddy soils Fixing atmospheric N 2 (B-G G algae) Some soil algae swim by flagella Soil Fungi Yeasts, molds, mushrooms 10-100 billion/m 2 Cell with a nuclear membrane and cell wall Most versatile & most active in acid forest soils Tolerate extremes in ph (bacteria do not) Mycorrhizae symbiosis Association between fungi & plant root Increased SA (up to 10 times) Increased nutrient uptake, especially P Mycorrhizae Fungi 1. Ions in solution 2. Movement from solution to root (diffusion) Phosphorous granule hyphae Root hair 7

Symbiosis Fungi provide nutrients Plant root provides carbon Ectomycorrhiza Root surfaces and cortex in forest trees Endomycorrhiza Penetrate root cell walls agronomic crops- corn, cotton, wheat, & rice 10-100 100 trillion/m 2 Single-celled organism Rapid reproduction Small (4-5 µm) Mostly heterotrophic Soil Bacteria N oxidation: nitrification NH 4+ NO - 3 S oxidation S + 3O 2 + 2H 2 O H 2 SO 4 N fixation N 2 NH + 4 rhizobium Oxygen, moisture, temperature, O.M., ph Benefits of Soil Organisms OM decomposition The most significant contribution N, S, & P nutrients Elemental transformations N (NH + 4 NO - 3 ) S (S SO 4 ), Fe (Fe 2+ Fe 3+ ) Mn (Mn 2+ Mn 4+ ) Nitrogen fixation (N 2 NH + 4 ) Algae: wetland Bacteria: legumes Breakdown toxic organics (bioremediation) Pesticide degradation: DDT Oil & gasoline degradation 8

Effect of Organisms on Nutrient Availability Soil Organic Matter Carbon Hydrogen Oxygen Phosphorus Nitrogen Sulfur Soil Organic Matter Biomass: Living organisms Detritus: Identifiable dead tissue Humus: Nonliving tissue Humic 60-80% SOM Complex Resistant Fulvic acid, humic acid, humin (Undefined, high molecular wt.) Nonhumic 20-30% SOM Less complex Less resistant Polysaccharides, proteins, acids (defined, lower molec. Wt.) 9