![]() | Soils, Crops and Fertilizer Use |
![]() | ![]() | About this manual |
![]() | ![]() | Acknowledgements |
![]() | ![]() | Chapter 1: Down to earth - Some Important Soil Basics |
![]() | ![]() | What is soil, anyway? |
![]() | ![]() | Why do soils vary so much? |
![]() | ![]() | Topsoil vs. subsoil |
![]() | ![]() | The mineral side of soil: sand, silt, and clay |
![]() | ![]() | Distinguishing "tropical" soils from "temperate" soils |
![]() | ![]() | Organic matter - a soil's best friend |
![]() | ![]() | The role of soil microorganisms |
![]() | ![]() | Chapter 2: Trouble-shooting soil physical problems |
![]() | ![]() | Getting to know the soils in your area |
![]() | ![]() | Soil color |
![]() | ![]() | Soil texture |
![]() | ![]() | Soil tilth |
![]() | ![]() | Soil water-holding capacity |
![]() | ![]() | Soil drainage |
![]() | ![]() | Soil depth |
![]() | ![]() | Soil slope |
![]() | ![]() | Chapter 3: Basic soil conservation practices |
![]() | ![]() | Rainfall erosion |
![]() | ![]() | Wind erosion |
![]() | ![]() | Chapter 4: Seedbed preparation |
![]() | ![]() | The what and why of tillage |
![]() | ![]() | Common tillage equipment |
![]() | ![]() | The abuses of tillage and how to avoid them |
![]() | ![]() | Making the right seedbed for the crop, soil, and climate |
![]() | ![]() | How deep should land be tilled? |
![]() | ![]() | How fine a seedbed? |
![]() | ![]() | Some handy seedbed skills for intensive vegetable production |
![]() | ![]() | Chapter 5: Watering vegetables: When? How Often? How Much? |
![]() | ![]() | It pays to use water wisely |
![]() | ![]() | Some common watering mistakes and their effects |
![]() | ![]() | Factors influencing plant water needs |
![]() | ![]() | Ok, so get to the point! how much water do plants need and how often? |
![]() | ![]() | Some methods for improving water use efficiency |
![]() | ![]() | Chapter 6: Soil fertility and plant nutrition simplified |
![]() | ![]() | Let's Make a Deal |
![]() | ![]() | How plants grow |
![]() | ![]() | Available vs. unavailable forms of mineral nutrients |
![]() | ![]() | Soil negative charge and nutrient holding ability |
![]() | ![]() | Soil pH and how it affects crops growth |
![]() | ![]() | Important facts on the plant nutrients |
![]() | ![]() | Chapter 7: Evaluating a soil's fertility |
![]() | ![]() | Soil testing |
![]() | ![]() | Plant tissue testing |
![]() | ![]() | Fertilizer trials |
![]() | ![]() | Using visual "hunger signs" |
![]() | ![]() | Chapter 8: Using organic fertilizers and soil conditioners |
![]() | ![]() | What are organic fertilizers? |
![]() | ![]() | Organic vs. chemical fertilizers: which are best? |
![]() | ![]() | Some examples of successful farming using organic fertilizers |
![]() | ![]() | How to use organic fertilizers and soil conditioners |
![]() | ![]() | Chapter 9: Using chemical fertilizers |
![]() | ![]() | What are chemical fertilizers? |
![]() | ![]() | Are chemical fertilizers appropriate for limited-resource farmers? |
![]() | ![]() | An introduction to chemical fertilizers |
![]() | ![]() | Common chemical fertilizers and their characteristics |
![]() | ![]() | The effect of fertilizers on soil pH |
![]() | ![]() | Fertilizer salt index and "burn" potential |
![]() | ![]() | Basic application principles for N, P, and K |
![]() | ![]() | Fertilizer application methods explained and compared |
![]() | ![]() | Troubleshooting faulty fertilizer practices |
![]() | ![]() | Getting the most out of fertilizer use: crop management as an integrated system |
![]() | ![]() | Understanding fertilizer math |
![]() | ![]() | Chapter 10: Fertilizer guidelines for specific crops |
![]() | ![]() | Cereals |
![]() | ![]() | Pulses (grain legumes) |
![]() | ![]() | Root crops |
![]() | ![]() | Vegetables |
![]() | ![]() | Tropical fruit crops |
![]() | ![]() | Tropical pastures |
![]() | ![]() | Chapter 11: Liming soils |
![]() | ![]() | The purpose of liming |
![]() | ![]() | When is liming needed? |
![]() | ![]() | How to measure soil pH |
![]() | ![]() | How to calculate the actual amount of lime needed |
![]() | ![]() | How and when to lime |
![]() | ![]() | Don't overlime! |
![]() | ![]() | Chapter 12: Salinity and alkalinity problems |
![]() | ![]() | How salinity and alkalinity harm crop growth |
![]() | ![]() | Lab diagnosis of salinity and alkalinity |
![]() | ![]() | Appendixes |
![]() | ![]() | Appendix A: Useful measurements and conversions |
![]() | ![]() | Appendix B: How to determine soil moisture content |
![]() | ![]() | Appendix C: Spacing guide for contour ditches and other erosion barriers* |
![]() | ![]() | Appendix D: Composition of common chemical fertilizers |
![]() | ![]() | Appendix E: Hunger signs in common crops |
![]() | ![]() | Appendix F: Legumes for green manuring and cover-cropping in tropical and subtropical regions |
![]() | ![]() | Appendix G: Some sources of technical support |
![]() | ![]() | Appendix H: A bibliography of useful references |
• Osmotic Effect of Salts: Soluble salts in the soil water reduce the ability of plants to absorb water through their root hair membranes (a process called osmosis). If the salt concentration is high enough, water actually starts moving out of the plant roots back into the soil, and the plant may soon die; this is called plasmolysis. At lower salt levels, plants may suffer leaf tip burn, stunting, and defoliation. Germinating seeds and young seedlings are the most sensitive to this osmotic effect. As shown in Table 12-2, crops vary considerably in their salinity tolerance.
• Effect of Sodium: Sodic soils harm plant growth mainly through the toxic effect of sodium itself, the high alkalinity (pH 8.5-10), and the toxicity of the bicarbonate ion with which the sodium is often associated. Germinating seeds and young seedlings are the most sensitive.
• Boron Toxicity: Most irrigation water contains boron which becomes toxic above 1-2 parts per million. Boron is not easily leached from the soil. Irrigation water with a high boron content may limit farming to boron tolerant crops. As shown in Table 12-3, crops vary considerably in their tolerance to boron.
• Rainfall-induced injury: If high evaporation and lack of sufficient leaching allow a high level of salts to accumulate at the soil surface over the weeks, an unseasonal, light rain shower cay move these salts only as far as the crop root zone and cause injury. This is mainly a problem on peat soils when sub-irrigation is used. (Sub-irrigation consists of running water down wide canals through the field to raise the water table enough to irrigate plants by upward capillary movement; It's commonly used on peat soils, which tend to have high water tables.)