Soil Types, Composition, Texture And Temperature
Akopọ
Pick up a handful of soil and you are holding a mixture: mineral grains of different sizes, dark humus, water, air and a teeming population of living things. The balance of these parts decides everything that matters to a farmer, from how much water the soil holds to how easily roots push through it and how warm it is in spring. Two fields side by side can grow very different crops simply because one is sandy and the other is clay.
In this lesson you will learn to describe a soil profile, sort soils by the size of their particles into sand, silt and clay, and recognise the prized crumb structure that humus helps to build. You will compare sandy, loam and clay soils, list the constituents that make up any soil, and see why soil temperature can make or break a young seedling.
Awọn Afojusun
- (a) describe soil profile in terms of topsoil, subsoil and underlying materials.
- (b) describe soil texture in terms of different sizes of soil particles, sand, silt and clay.
- (c) understand soil structure, including the importance of forming and maintaining a good crumb structure, the effects of humus and maintenance of organic matter in the soil, oxidation of organic matter and the loss of soil structure causing capping and soil pans.
- (d) describe different soil types (sandy soils, loam soils and clay soils) and their properties, including water-holding capacity and drainage.
- (e) outline soil constituents in terms of mineral matter, organic matter, air, water (free or gravitational water, capillary and hygroscopic water) and living organisms (bacteria, nematodes, fungi and earthworms).
- (f) understand the influence of soil temperature on the rate of plant growth, the danger of excessive heat to young seedlings and the danger of frost to some crops, and the methods of reducing the effect of extreme temperatures by mulching of seedbeds and shading of transplanted seedlings.
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Ìdánwò Ẹ̀kọ́
Oriire fun ipari ẹkọ lori Soil Types, Composition, Texture And Temperature. Ni bayi ti o ti ṣawari naa awọn imọran bọtini ati awọn imọran, o to akoko lati fi imọ rẹ si idanwo. Ẹka yii nfunni ni ọpọlọpọ awọn adaṣe awọn ibeere ti a ṣe lati fun oye rẹ lokun ati ṣe iranlọwọ fun ọ lati ṣe iwọn oye ohun elo naa.
Iwọ yoo pade adalu awọn iru ibeere, pẹlu awọn ibeere olumulo pupọ, awọn ibeere idahun kukuru, ati awọn ibeere iwe kikọ. Gbogbo ibeere kọọkan ni a ṣe pẹlu iṣaro lati ṣe ayẹwo awọn ẹya oriṣiriṣi ti imọ rẹ ati awọn ogbon ironu pataki.
Lo ise abala yii gege bi anfaani lati mu oye re lori koko-ọrọ naa lagbara ati lati ṣe idanimọ eyikeyi agbegbe ti o le nilo afikun ikẹkọ. Maṣe jẹ ki awọn italaya eyikeyi ti o ba pade da ọ lójú; dipo, wo wọn gẹgẹ bi awọn anfaani fun idagbasoke ati ilọsiwaju.
- Which soil particle is the largest? A. Clay B. Silt C. Sand D. Humus Answer: C
- Clay particles have a size of: A. More than 2.0 mm B. 0.05 to 2.0 mm C. 0.002 to 0.05 mm D. Less than 0.002 mm Answer: D
- Which soil type generally has the best balance of drainage and water-holding for most crops? A. Pure sand B. Loam C. Pure clay D. Gravel Answer: B
- The water held in the small pores of the soil and available to plant roots is: A. Gravitational water B. Capillary water C. Hygroscopic water D. Free water Answer: B
- A hard crust formed when heavy rain seals the surface of bare soil is called: A. A soil pan B. Capping C. A crumb D. Humus Answer: B
Ṣiṣẹ́ lórí àwọn ìbéèrè wọ̀nyí nínú ohun èlò náà
Ṣiṣẹ́ lórí àwọn ìbéèrè wọ̀nyí nínú ohun èlò náà
Awọn Iwe Itọsọna Ti a Gba Nimọran
Ẹ̀kọ́ síwájú láti àwọn orísun ṣíṣí
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Abala ìwé ẹ̀kọ́
The Soil
Describe how soils are formed
"Biology: The Soil" by OpenStax, OpenStax, Rice University, licensed under CC BY 4.0 (https://creativecommons.org/licenses/by/4.0/). Source: https://openstax.org/books/biology/pages/31-2-the-soil. Access for free at https://openstax.org/books/biology/pages/1-introduction
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