☰ Contents · Geography

The Mirzachol natural-geographic district

Lessons 50–51 · 2 lessons · P. Gulomov, H. Vahobov, P. Baratov, M. Mamatqulov. Geography (Physical Geography of Central Asia; Physical Geography of Uzbekistan), Grade 7. Revised and expanded 5th edition. “O‘qituvchi” Publishing House, Tashkent, 2017
51

Climate, waters, soils, plants and animals (Mirzachol)

Textbook: pp. 124–125
GoalDescribe the climate, waters, soils, plants and animals of the Mirzachol district.
New words
thermal low · termik depressiyaevaporation · bug‘lanishsalinisation · sho‘rlanishAydar-Arnasay lake system · Aydar-Arnasoy
Explanation

In winter cold air from the Arctic and Siberia enters the plain unhindered and collects there, unable to cross the southern mountains: the January mean is –1…–3°C and some days reach –30…–35°C. In summer, under a thermal low, the air is dry and scorching: the July mean is +26…+28°C and the hottest days +44…+45°C. Annual precipitation on the plain is 200–350 mm and increases towards the mountains, while possible evaporation is 1000–1200 mm, about 4–4.5 times the precipitation. The main water source is the Syrdarya, whose valley is up to 15 km wide. The Sangzor is fed by snow water and the Jizzakh reservoir regulates its flow. Aydar-Arnasay is the largest lake system in Uzbekistan: it appeared in 1969–1970 when the Syrdarya was in high flood and a huge volume of water was released from the Chardara reservoir. On the plain ground water lies close to the surface (1–5 m), is salty and undrinkable, so saline soils are common. Most soils are irrigated light grey and grey-meadow soils. Plants: ephemerals, wormwood, sora, tamarisk, camel-thorn; in the foothills barberry, rose, pistachio and almond, walnut in the Nurata and juniper at 1500–2500 m in the Turkestan range. Animals: jerboa, ground squirrel, fox, wolf, gazelle; in the tugai jungle cat, boar and pheasant; in the mountains deer and ibex.

Worked examples
On a scorching July day in Mirzachol, working in the morning and evening instead of at midday reduces harm from heat.
In a field where ground water is at 1–2 m, moisture rises to the surface, evaporates and leaves salt behind: the field becomes saline.
Class activity

“Salinisation experiment”: pour salty water into soil in a large container, put it in a sunny place and after a few days observe the white layer on top. Do not drink the salty water and work with an adult.

Practice
1
Why are there very cold days in Mirzachol in winter?
2
How did the Aydar-Arnasay lake system appear?
3
If precipitation is 250 mm and evaporation 1000 mm, how many times more is evaporation than precipitation?
4
Why does soil become saline when ground water is near the surface?