TY Btech Syllabus-16sept09
Purpose: To provide participants with an understanding of the sinks of carbon and sources of methane and nitrous oxide emissions in land based systems.
Deserts
41. soil components and their properties by allah dad khan
ASTM .D2216wc.pdf
Siklus NPK
STRUKTUR TANAH. Soil Structure Structure – arrangement of individual particles in relation to each other. Soil structure is the arrangement of particles.
Different soil types develop in different climates. Soils-4-1 Image: T. Loynachan.
Desert Soils. Deserts can be HOT or COLD. But they are all very DRY. All deserts have more evaporation then rainfall. Deserts cover 20-35% of the Earth’s.
Biome characteristics. Quick Recap… As latitude gets higher Less direct sunlight More seasonal variation Extreme changes in day / night at poles.
Chapter 7 Weathering and Soil 7.2 The nature of soil notes sheet.
Soil Not just dirt!. Soil… is a thin surface layer of the Earth’s crust. is affected by agents such as weather, wind, water, and organisms. is (approximately)
