Vologі subtropics roztashuvannya natural zones. Runtivological subtropics
The runts of the subtropics are represented by two types: Chervonozem and zhovtozemi, Zagalna square which to become close to 0.6 million hectares. The stench of expansion in the Transcaucasus and occupy two additional layers, one of Chornomorskiy Uzbek, Інshiy - bilya of the Uzbek coast of the Caspian Sea in the region of Lankaran.
factor of soil satisfaction... Climate and warmth with an equally hot summer and meak, with cold frosts, charge. The average temperature is 13-14 ° С, and the period from the temperature below 10 ° С becomes 240-250 days. Rik vipadaє 1500-2500 mm and more falloff, which is a zooming type of water regime. Come on, be angry in nature, it's a great part of the fall and winter.
Relief is typical for the front and strong dismemberment, but with the angry nature of the fall, the intensive development of water erosion.
Overloads soil-supporting rocks- red-colored and yellow-flowered bark of vivitryuvannya. Persha is represented by argillaceous-worm-loamy eluvia of the main weathered rocks (trachity, basalt, andesite), and the other is represented by eluvia of the dark-yellow colora of sedimentary rocks (clay shale, piskoviki). The need for the cich to become 2-10 m and more.
Roslinnity is represented by written subtropical forests... They cross over oak, hornbeam, chestnut, maple, cherry laurel, rhododendron, which are not often intertwined with lianas. Organic litter of organic matter reaches 20 tons per hectare; with it, up to 800 kg per 1 ha of nitrogen and ash elements are turned into the ground.
Worm-earth and zhovtozem are formed as a result of active biochemical processes that occur in a sour middle. Intensely and even warmly climate with an intensive spreading of organic mass practically by stretching out to rock. When humus falls off the humus, trocha accumulates in the soil, and the fraction of fulvic acids is re-fermented in the storehouse. Visiting the great class carbon dioxide gas This is the result of an intensive deployment of an organic siege and the development of a roslin, a sprinkling of an energetic destruction of the mineral part of the runt. A deep drop of aluminosilicates is supervised to increase the amount of calcium, magnesium, and also partly silicon and saline. Remain and produce breeds characteristic of a red-headed barnacle (name and name). At the same hour, biological accumulation of calcium, phosphorus, water and other elements, such as dzherel food for roslin, is added to the soil in the humid horizon.
On the ground in vologic subtropics іstotno pouring in chemistry warehouse mothers.
Chervonozem was formed on the red bark of vivitryuvannya, which is strongly affected by the presence of (1-2%), it is replaced by trochas, silica (35-40%) and is filled with sesquioxides (50-60%). The process of podzolization, which is characteristic of the soil-dissolving in the sour middle, is even weak in the chervonozems.
The upper horizons of chervonozems are located close to 5-8% humus, 0.2-0.4% nitrogen and 0.1-0.2% phosphorus. I do not perevischuyu 15-20 mg-ZKV per 100 g of soil. Claying cations of trocha Ca and Mg, and H and A1 occupy 60-75% of the amount of clay. To this, the reaction of chervonozem is strongly acidic (pH of the water layer is 4-5). However, chervonozems are made up of good agrophysical power, zooming in with a significant world, an important mechanical warehouse and a water-resistant structure in the the same role cover with sesquioxides.
Zhovtozemi is formed on yellow-colored barks of vivitryuvannya, yak, on vidminu from chervonokolіrnoyu, to take a lot more (2-5%), less sesquioxides (20-30%) and more silica (40-60%). The process of podzolization of bends here is much stronger, so in the profile of the zhovtozem it is clear to see the podzolization horizon tighter up to 60 cm and illuvial, so to take revenge on the abundant ortsteine concretions.
Zhovtozemi are often taken over by the authorities of the chervonozems. At the humus horizon, the stench replaces less humus (3.5-5%), and from clayed cations, it takes Ca and Mg (75-95% of the clay). However, in the clayed mill there is a sludge of water, which will accumulate a weakly acidic reaction of soils (pH of a water layer is 5-6).
It's easy to add your good robot to the knowledge base. Vicorize the form
Students, postgraduates, young people, who are victorious to develop the knowledge base in their own lives and robots, will be your best friend.
Posted on http://www.allbest.ru/
plan
soil of vologic subtropics
1. Understanding about the soil of vologic subtropics
2. Silskogospodarske vikoristannya
3. Features of the runthological subtropics
literature
1. Understanding about the soil of vologic subtropics
The runthological subtropics are represented by two types: chervonozems and zhovtozems, the back area of which becomes close to 0.6 million hectares. The stinks are wider in the Transcaucasia and occupy two areas, one of which is widespread on the Chornomorsk Uzbek coast, and the other is the Uzbek coast of the Caspian Sea in the area of Lankaran.
Soil-Satisfaction Factor. Climate and warmth with an equally hot summer and meak, with cold frosts, charge. The average temperature is 13-14 ° С, and the period from the temperature below 10 ° С becomes 240-250 days. Rik vipadaє 1500-2500 mm and more falloff, which is a zooming type of water regime. Come on, be angry in nature, it's a great part of the fall and winter.
Relief is typical for the front and strong dismemberment, but with the angry nature of the fall, the intensive development of water erosion.
It is important for soil-producing species - red-colored and yellow-flowered bark of vivitryuvannya. The persha is represented by the argillaceous-worm-like clayey of the main weathered rocks (trachity, basalt, andesite), and the other is represented by the dark-beaked wormwood of sedimentary rocks (clay shale, piskoviki). The need for the cich to become 2-10 m and more.
Roslinnity is represented by subtropical forests... They cross over oak, hornbeam, chestnut, maple, cherry laurel, rhododendron, which are not often intertwined with lianas. Organic litter of organic matter reaches 20 tons per hectare; with it, up to 800 kg per 1 ha of nitrogen and ash elements are turned into the ground.
Worm-earth and zhovtozem are formed as a result of active biochemical processes that occur in a sour middle. Intensely and even warmly climate with an intensive spreading of organic mass practically by stretching out to rock. When humus falls off the humus, trocha accumulates in the soil, and the fraction of fulvic acids is re-fermented in the storehouse. Viriznyaetsya at a great amount of carbon dioxide gas, as the result of the intensive deployment of the organic siege and the development of the roslin, with the energy rushing of the mineral part of the runt. A deep drop of aluminosilicates is superfluous to higher levels of calcium, magnesium, and also partial silicon and saline. Remain and produce breeds characteristic of a red-headed barnacle (name and name). At the same hour, biological accumulation of calcium, phosphorus, water and other elements, such as dzherel food for roslin, is added to the soil in the humid horizon.
The chemistry warehouse of the mother's breeds is poured into the soil at the natural subtropics.
Chervonozem was formed on the red bark of vivitryuvannya, which is strongly affected by the presence of (1-2%), it is replaced by trochas, silica (35-40%) and is filled with sesquioxides (50-60%). The process of podzolization, which is characteristic of the soil-dissolving in the sour middle, is even weak in the chervonozems.
The upper horizons of chervonozems are located close to 5-8% humus, 0, 2-0, 4% nitrogen and 0, 1-0, 2% phosphorus. I do not perevischuyu 15-20 mg-ZKV per 100 g of soil. Claying cations of trocha Ca and Mg, and H and A1 occupy 60-75% of the amount of clay. To this, the reaction of chervonozem is strongly acidic (pH of the water layer is 4-5). However, chervonozems are made up of good agrophysical powers, zoomed in with a significant world and an important mechanical warehouse and a water-resistant structure in the established role of sesquioxides.
Zhovtozemi is formed on yellow-colored barks of vivitryuvannya, yak, on vidminu from chervonokolіrnoyu, to take a lot more (2-5%), less sesquioxides (20-30%) and more silica (40-60%). The process of podzolization of bends here is much stronger, so in the profile of the zhovtozem it is clear to see the podzolization horizon tighter up to 60 cm and illuvial, so to take revenge on the abundant ortsteine concretions.
Zhovtozemi are often taken over by the authorities of the chervonozems. At the humus horizon, the stench replaces less humus (3, 5-5%), and from clayed cations, Ca and Mg (75-95% of clay). However, in the clayed mill there is a sludge of water, which will accumulate a weakly acidic reaction of soils (pH of a water layer is 5-6).
2. Silskogospodarske vikoristannya
Silskogospodarske vicorystannya chervonozem and zhovtozemi. Climate of vological subtropics of Velmi is friendly for the processing of valuable crops: ethereal, citrus fruits, tea plants and others.
The most important values in the zone should be followed by calls, we will direct them to fight against water pollution.
Intensive culture of bagatokh roslin on red soil and zhovtozems can only be obtained with the systematic introduction of large doses of organic and mineral goodness. Vapnuvannya on black soils and zhovtozems is required only for the cultivation of such crops, yak citrus, corn.
The subtropics of the subtropics are trivial warm litom and a short soft winter.
Vologі subtropics are rich lands, friendly for vegetable crops. For example, the trivial period of vegetation and high summer temperatures at the first gathering of the United States is favorable for the growth of such crops as sweet potato, kvass and din. As a matter of fact, spring and autumn meats allow you to cut off two crops of such vegetables, yak spinach, greens, radishes and kvass. Hanging up tomatoes, peppers and celera. At the same time, there is a great deal of industry in the development of sheep and goats for the production of new states in the United States.
Development of dry and vologic subtropics.
Vologue subtropics are formed in a warm and warm climate. The number of fallen leaves behind the rocks rises between 1000 - 2500 mm. Overwhelm the autumn and winter fallen, as a rule, an angry character.
Silskogospodarske victoriannya of soils in vologic subtropics.
The zone of vologic subtropics is most suitable for tea culture. The price is explained by friendly soil and hydrothermal minds. The acidic reaction of chervonozems and zhovtozems, and there is not a large number of positively associated with the productivity of the tea bush, which normally grows only on acidic soils, and on luggy guineas. It was shown before the storage of rugged cations in soils and crops of tea plantations in Georgia that it is necessary for the normal development of the tea bush to grow in the soil of A.
The runts of the subtropics may not be satisfactory physical and chemical authorities, You can polishit the contributions of organic goodies. Ale delivery to large plantations to nav and small quantities of pus is hampered in conjunction with the girskiy relief of micevost. In the tsikh umovah, the meaning of the green is good, yak, I do it, I don’t get pus, I grow up. In addition, grow green manures to seize plantations, roztashovani on graves, from the age and preserve at old boards from vimivannya from - the soil of the cultivated living elements.
The natural minds of the subtropics of the Velmi are friendly for the production of bagatokh of the Sylkogopodar cultures. Tea bushes, citrus and essential oil cultures, tyutyun and іnshі silskogospodarski roslini grow on the red soils and zhovtozems. Alle tsі soil may have a small supply of lively chapters available for the roslin. Crumbling forms are easily absorbed by nitrogen from the upper horizons, and there is a large number of one and a half oxides to rob the soil of phosphates that are inaccessible to the roslin.
3. Features of the soil in the subtropics
In zones of vologic subtropics, water erosion is strongly manifested.
Low-lying zone of vologic subtropics with a warm winter and a warm summer; breezes are spared during the seasons and rock, especially often in lіtnі mіsyatsі... The zone extends for 3 pidzones.
Near the coastal zones of the natural subtropics of marine salts, they take brittle aluminum, just to witness the conduct of the process.
Vlіtku in areas vologicheskogo subtropics can reach trivial period with a lack of number of fallen, if the greenbacks are planted in wide rows of bagaturian nasadjens, living in a vologue with a root, you can bring a base. The top of the plantation is repaired from spring to mid-spring; korisno mulchuvati soil, I would like to be in the near-boil circles, mowed with a green mass of siderates. Light green, kindly autumn, often in early spring.
Near the regions of the zh vologic subtropics, winter will be more intense, with more frosty weather during the day, because of the average temperatures of the coldest month, it is close to 5, z great number fall.
Nybilsch by broadening soil-forming rocks of the vologic subtropics girskikh breeds: Andesites, basalts, porphyritic guffs and sedimentary theoretical deposits - clay and rich-clay shales. On larger low territories, aluvial and deluvial-proluvial clay-pebbles and pebble-boulders are used as soil-forming rocks.
In the minds of the coastal zones and vologic subtropics in case of atmospheric corrosion, it is possible to establish a number of stages and development, the most important stage. At the second stage, it is a great inflow to repair houses and meteorological parameters. At the onset of the stage, if corrosion products take place on the surface of the metal, at the lower critical level, the activity of the houses decreases.
The hydrochemical regime of the sea in the minds of the subtropical subtropics is especially important from the point of view of atmospheric corrosion of metals, especially in the case of Russian winds from the sea to land. Instead of chlorides, the appearance of sourness, salinity and salinity sea water, Most of the other factors, є by the final characteristics of the hydrochemical regime of the sea. As a result of the development of materials from the Batumi meteorological observatory, it was established that in the region of Batumi, instead of chlorides, and the salinity changes little by a stretch of rock: it is a little more likely to turn on the gray water. change, move slowly.
Galvanic coverage in the coastal zones of the biological subtropics is found in the greater minds of the higher temperatures and the average temperature and salinity of the weather, the frequency of the feeling of intense sleepiness.
Runti, widened in the regions of the natural subtropics of Transcaucasia. Physical power and the structure is friendly. Demand for the humus horizon grows 25 - 40 cm. Opozo-lennge K. May increase acidity, less humus and weaker populations. The range of clay is 10 - 15 meq per 100 g of soil. Require vapnuvannya і introduced additional doses of mineral (especially phosphoric) kind, sucked with pus and green kind. It is also necessary to counter the agrotechnics.
From Tuapse to Sochi, the region of vologic subtropics is being repaired. Up to the valley of the Ashe rivulet, there is a little nord-ost inflow, there is access to dry continental winds of the curtains along the ridge of mountain ridges. The temperature is higher, the weather is higher in winter, the volume is great and the number of years of the dormouse is great, and the subtropical height is growing for the exuberant growth.
For tea - the main culture of the zones and subtropics of the western part of the Georgian PCR - on the red soil, the velmi is effective nitrogen and phosphorus good. The increase in the collection of green tea leaves as a result of the introduction of great goodness is encouraged to grow on plantations for 10 years and more.
The installation of indexes of the same microelements on some soils of the same subtropics, in fact, is minimal.
Geochemistry and ecology of naphtha flows in zones of vologic subtropics / / Migration of wandering rivers in soils and summers: Mater.
The fourth zone includes the Baltics (IV A), the subtropics (IV B), Primor'i and Sakhalin in lіtnіy period... Winter is a zone of beef, albeit with an advanced logos.
For a correct assessment of the corrosive aggressiveness of the most characteristic climatic regions of the same subtropics in the toy subtropics, five special viproboval majdanchiks were installed in the territory of meteorological stations (Fig. II. Steel patterns, exhibited in Kobuleti (70 - 80 m from the sea), were given the strongest corrosion.
Near the Lankaran and Astara regions of the Skhidny Transcaucasia, there is a growing climate of subtropical subtropics in the minority. The power of the climate of the whole district is allowed to be called the climate of the same subtropics. During the summer in Lankaran-Astara region, the weather is more dry and wet, and humid weather is more frequent.
Climat to the Menji resort is worn in a weakened step of rice subtropics.
Corrosion in cracks and gaps is most important in the coastal zones of natural subtropics, corrosion products are replaced by chlorides and sulfates, and they can be used to dissipate crumbled metal.
Mastila GO54 and GO54P quickly hang, їх stasis in the minds of vologic subtropics does not give positive results, besides, the stench is unstable against fungi.
For the red-earth and pidzolic soils in the subtropics of Georgia, the dose of vaping should be adjusted according to the data of the exchange acidity.
Bagatorial data of the Batumi zonal meteorological observatory on the outskirts, the most characteristic regions of the natural subtropics (Batumi, Kobuleti, Keda), as well as the dynamics of meteorological parameters that are not of a certain order
In the climatic lifestyle of Batumi and its outskirts, it is characterized by folding meteorological contrasts, the most typical for vological subtropics. The increase in the salinity of the coastal atmosphere due to the increase in the temperature and the temperature is aggressive in the middle, which can lead to intensive corrosive deterioration of materials.
In 1967, an agrochemical cartogram was stored for the exchange of magnesium for the oldest government in the subtropics of Georgia - the Salibaurok tea house of the Batumi district. From the pictures of cartographers it can be seen that on the bagatokh dilyankas of the state of the tea and citrus culture, the introduction of magnes is good. However, є dilyanki, de vmіst іmіnіyu a whole lot for the vivification of the tea bush, which is backed up with a relf, a mechanical storage of soil and a complex of agrotechnical calls, as there were a number of rocks here. Zvidsy can be built up, but the thought about the widespread stagnation of magnivih kindly on the old tea plantations is not justified. Mi vvazhaumo, for storing magnes, kindness is needed for a good differentiation.
In the zones of dry subtropics of the subtropical class of zonation, there is widening of the hirski syrozem and brown soil, and in the zones of vologic subtropics, the lower belt of representations of the chervonozems and zhovtozems.
Climatic zonality is poorly rotated, on a large part of the Russian platforms there is a similar climatic setting, which is full of modern subtropics. Tilki on Extreme Pivnochі climatic mind close to the dead. A hot і vologous climate, mlyaviy tectonic regime is set up on the flat waters of the strained barks of the chemical vivification of the kaolin and bauxite warehouse, which were saved by miracles at the Ukrainian crystal massif. Approvals, thin pischano-silty-clayey material spread by leaks over the great area of the milky sea, which is covered by the Russian platforms. In the main, in the early Paleogene, there were deposits, peaks, often glauconite, and later - clays. Marl and purely carbonate litter are formed only in the glide-water part of the Black Sea depression. In the Volga region of the Priural, there is a triple accumulation of terrigenous-kremian formations.
In the laboratory, the development of robots was carried out for the purpose of adding: mineral, manganese and zinc in different soils of natural subtropics following the method of Peive and Rinkis. The results of this period show that in red-earth soils, instead of manganese, growth and variation from 25 to 45 mt per 1 kg of air-dry soil; in the carbonate soils of Zakhidniy Georgia, manganese is not revealed.
In the world of sunshine for the day, as a result, there is an increase in the direction of the Head Caucasian Ridge of Klimat Nabuvian Rice, ruling the region of the natural subtropics. It should be manifested in a small change in natural conditions. skidnykh vіtrіv, In the majority of falloffs (for example, js Tuapse is a normal number of falloffs to become 1200 mm) and of the same amount of falloff.
It is widespread to become stagnant in the quality of technical vaseline (mastilo UN), having appeared as an insufficiently good preservative in the minds of the subtropics.
Mastila ЦІАТІМ202, ЦІАТІМ203, МС70, PVK with AKOR1 additive, MC20 oil with AKOR1 additive in the minds of high subtropics will give a good finish and with success it can be recommended for tropics.
Sochi resort area with great natural political authorities in the long run: warm water chloride-sodium mineral water, soft climate of natural subtropics, warm sea. All parts of the Sochinsky resort area are allocated from the snowy descent and the lancey outcropping of the high mountain ranges of the Head Caucasian Ridge; burn down, step by step, descend like an amphitheater to the very shore of the sea, seizing all the coastal smog through the access of cold and cold weather. The coastal mountains up to the snowy peaks are covered with rich growth - beech, hornbeam, chestnut and coniferous forests.
It is located in the mid-mountainous zone of Adjara, 28 km from Batumi, at a height of 1200 m above the sea level, characterized by a climate of natural subtropics with alike cold winters and altogether warm summer. number sleepy days and the number of fallen is not important here.
On the Caucasian Uzbek coast of the Black Sea and in the Western Georgia, the soil is grown, grown in chervonia, brown and zhovty color; tse runt vologic subtropics.
The Azov Sea and the private part of Chorny are located in Pomirniy Zones, Pivdenna - in the zone of the subtropical climate of the Middle Sea type, the private-skid part - in the zone of vological subtropics.
To that, in the classification of the naming of rural resorts, a reference (in addition to equilibrium) to the nature of growth and belonging to the main climatic zone, For example: Rizke Uzmor'ya - Rivninniy, seaside resort of Lisovoy zone; Sukhum is a seaside resort of humid subtropics.
The main zones of stagnation of green goodness of the onset are: a) pivn_chna non-corn-earth zone - areas of sufficient flooding with soddy-pidzolic soils, as well as gray fossil soils, a wide line of grassy soil; b) all growing regions with low-humus soils (syrozems of Middle Asia, storms and brown soils of the Volga region and other regions), regions and forest-steppe zones with gray fossil soils and hardened Chornozem soils and c) vology sub-regions
It’s viciously weepy in winter, and also the area is very safe for warm and vologo during the period of active vegetation to grow it as a valuable area for the development of subtropical crops. The region of the natural subtropics of Velmi is friendly and for the development of resorts;
The runts of the wider subtropics in Transcaucasia, along the Uzbek coast of the Black Sea in the Georgian RSR. Chervonozem and zhovtozemi vologic subtropics in the Radiansky Union occupy 0 6 million hectares.
Here the climate of the position is seen in the logical subtropics, the winter is still coming and there is a great number of fallen in the midst of the rock.
The zone is rich in roslinn_styu, the power of the climate of vologic subtropics, foxes from the pine trees, as well as the third roslinn_ of the Middle Sea climate.
Tea shrub grows good only in the regions of the natural subtropics of Georgia, Azerbaijan and Krasnodar Territory... Mineral goodness may be the most significant in the rejection of high tea leaves.
List of Victory Literature
1. Geography. The encyclopedia is now well illustrated. - M .: Rosmen. Edited by prof. A.P. Gorkin. 2006.
2.Runti SRSR. M., Dumka, 1979
3. Dobrovolskiy VV Geography of soil with the basics of soil knowledge. M., Vlados, 2001.
4. Glazovskaya MA, Gennadiev AN Geography of soil with the basics of soil knowledge. M., Moscow State University, 1995
5.http: //mse-online.ru/pochva/pochvy-vlazhnyx-subtropikov.html
Posted on Allbest.ru
...more documents
Growth of the main part of the equatorial forest. Equatorial Lisy Amazonia. Features of the growth of natural and changeable leaves. Vologі vіchnygіlі lіsy ekvatorіalnoy Africa. The head signs of the equatorial leaves, flora and fauna.
presentation, donations 10/27/2014
The peculiarities of the natural minds of the regions are extended to the logical equatorial and post-mortem tropical forests... Main natural resources to the region of the Malaysian Archipelago and the victorious people. Ecological problems, Hoes and ways of seeing.
robot course, additions 06.11.2013
Climate, reliability and relativity of the Astrakhan region. Soil-forming rocks and zones and rosters. Classification, budov, power of runts. Peculiarities of common brownish soils with light chestnut, salt licks and salt marshes. Priyomi p_dvischennya rodyuchost_.
abstract, additions 12/17/2014
Powerfulness of pidzolic soils of the Tom-Obsk interirichchia, formed on sharuvate, rich-supine rocks. Injection of the structure onto the mold and development of the soil. Climat, high quality, parent rocks, Hydrographic hem. Methods for the detection of soil.
robot diploma, additions 06/26/2013
Geographic location of the Apenninsky pivostrov. Factor of soil-satisfaction: soil-making breed, relief, living organisms, klimat and hour. versatility ground cover Apenninsky p_vostrov. Victorian soil and ecological camp.
control of the robot, additions 01/03/2011
Іstorіya vivchennya burikh fossy soils. Determine the formation of burozems and areas of expansion. Geological budova and parent rocks. The main climatic data on the areas of widening brown fossil soils, their genesis and classification.
robot course, additions 04/26/2011
The zone of changeable areas, including monasteries: geographic location, natural mind, Roslinny i tvarinny svit... Shroud and Ridkolisya zone. The zone of vologic ekvatorialnyh lisiv, the problem of the virus. Zmіna shroud pіd injected vipasu.
course robot, additions 12/29/2012
Physical-geographic characteristics-class: cherguvannya vologicheskikh ekvatorialnyh masters and dry pasats charged; soil. Roslinny and tvarinniy light in the Canaima park. Hydrography: Riki, Angel-nayvishny waterfall in the light.
abstract, additions 20.11.2007
presentation, donations 03/15/2015
Fundamentals of the soil-geographic region Take a quick look at the classification of soils and soil cover. Understanding the structure of the soil cover. Physical and geographic characteristics, climate, height, relief, soil-forming species.
In the fringes of subtropical climatic zones in the rural parts of the continents, there are regions, de average temperatures are approximately the same, and a few falloffs and the mode of reading vary depending on the type. This rank, they see dry and vologue subtropics. Vlіtku in cikh areas panuyut tropіchnі disastrous masi, And the charge - the wandering of the masses of the other latitudes.
for backward parts The continent with the so-called Mediterranean type of climate is characterized by a spicot and dry summer (up to + 30 ° C) and a cool windy winter (the average amount of fallen leaves is 400-600 mm). In these areas, hard leaves and chagarniki grow. Vony is widened in California, Chile, Pivdenniy Afritsa, Aleksei are widely represented in the Middle Sea and Australia.
There are abundant types of trees and chagarniks in these forests, as well as hard leaves, covered with glistening wax nalot, some of the pubescence below. Korenev's systems and actions of the Roslin penetrate great glybin: For example, the root of the stone oak can reach the horizon of the underground waters, which is roasted on the clay close to 20 m from the surface of the earth. In Seredzemnomoria, there are native boules of vichgreen hardwoods from laurel, sycamore, olive trees and crushed stone and bark oak. From the light woods, from the good growth of chagarniki and grassy tiers, a rosy brown soil was formed, a great ball of humus was formed. For a long time, people have been engaged in farming in cikh mіstsy, and at once the part of the viruban foxes is significant, the unoccupied landscapes in the mayzhe have not been overshadowed. The lowlands of the coastline were occupied by pastures, olive and citrus trees, vineyards, fields of Troand and lavender. And there, de nemay have grown that nasadzhen, developed chagarnikov formations, called "maquis". They are characterized by growing trees, heather, duckweed, sunichna tree, olive, ryzhkov tree, myrtle, fistashka. Bagato lipocytes, legumes, rosots, clearly see essential oils.
In the midst of the people, de Pozhezha, there is an intensive agricultural activity.
Australian hardwood foxes, rosted on the ancient and western outskirts of the mainland, adopted by a number of species of acacia and eucalyptus (there are 525 species in Australia) Australian foxes are light and green foxes, with a good layer of chagarniks from legumes (more than 1000 species), myrtle and protean.
In the skid parts of the mainland in the boundaries of the subtropical climatic belt(For example, at the meeting for China, for the first time for the United States and for the first time in Brazil) vologі lіsi... Winter monsoons bring drier and colder winds from the inner parts of the mainland, and summer monsoons come at once with warmth - in the winds, which are cloudy from the ocean and dead ends. All in all, from 1000 to 2000 mm, the fall, and the ground water and flood occasionally slightly, fall from 1000 to 2000 mm. In cich regions on zhovtozems and red earth soils, they grow high-bumpy green foils, like deciduous, and even green. Here you can see rich old-time types of holonose roslin, for example, ginkgo, cryptomeria, metasequoia, cycad. Widened oaks, laurels, tea, rhododendrons, bamboo and liani. Great freedom is seen and created by the light of the monsoons. However, in Danish hour, a large part of tsikh lis_v was built, and at їkh m_stsi fields and pastoralists sprang up.
The olive, or the olive tree, is one of the most abundant cultivated growths. There are close to 60 different types of olive, albeit gospodarske value of the olive, the olive is cultivated, or the olive is European. Її to grow in areas with dry and warm climate - on the pivnichniy uzberezhzhi Midland Sea, In the Crimea, in the Caucasus, as well as in Central Asia and in Africa. A green tree, or a chagarnik tree with a height of up to 10 m, grows by and large, but it is alive and well - the average triviality of life is close to 300 rocks, the maximum - up to 2000 rocks. The growth of the tree is even more malovnichi zvdeyaki we will interweave the stoves with cracked bark and round dense crown with other sirly shky leaves.
Olive knew the glory of the whole world because of its fruits. The fruit of an olive tree is a custard with one seed, oiled with oily pulp. The pulp of olives has a lot of oil, calories and without vitamins. The siri fruits of the girky and the unfortunate, but in a long time ago people came to conserve them. In the main olive trees are used to remove oil.