Characteristics Of Soil Environmental Bonitovaných Units

Original Language Title: Charakteristika bonitovaných půdně ekologických jednotek

Read the untranslated law here: https://portal.gov.cz/app/zakony/download?idBiblio=47056&nr=327~2F1998~20Sb.&ft=txt

327/1998 Sb.



DECREE



The Ministry of agriculture



of 15 November 2004. December 1998,



laying down the characteristics of the soil and environmental bonitovaných

units and the procedure for their management and update



546/2002: Sb.



The Ministry of agriculture lays down, pursuant to section 8 (2). 8 of the law No. 284/1991

Coll., on land and land offices, as amended by Act No.

38/1993 Coll. and Act No. 217/1997 Coll.:



§ 1



Characteristics of soil environmental bonitovaných units



Bonitovaná soil-ecological unit (hereinafter referred to as "BPEJ") ^ 1)

characterized by climatic region, the main soil unit

sklonitostí and exposure, skeletovitostí and depth of soil which specify

the main soil and climatic conditions of the land, taking an investigational



and the climate, the region includes territory) with about the same climate

conditions for the growth and development of agricultural crops, according to annex No 1; is

the first digit is a five-digit number expressed as a code ^ 1) (hereinafter referred to as

"code number"),



(b)) the main soil unit is purposeful grouping of soil forms

related properties, which are determined by the genetic soil type,

subtype, půdotvorným substrate, grain, soil depth, degree of

hydromorfismu, or a distinctive sklonitostí or morphology of the terrain and

zúrodňovacím measures, in accordance with Annex 2; It is expressed as the second and third

digit numeric code,



(c)) sklonitost and exposure to the cardinal describes the formation of the surface

agricultural land according to annex No 3; the fourth digit is represented

a numeric code that is the result of their combination,



(d)) skeletovitost, which means the share of gravel and stone content in ornici to

the content of gravel and stone in straight-up to 60 cm, and depth of the soil, according to the

Annex No. 4; the fifth digit is represented with a numeric code that is

the result of their combination.



§ 2



Leadership BPEJ



(1) BPEJ are uniformly kept ^ 2) in numerical and cartographic representation of the

a nationwide database of BPEJ (hereinafter referred to as "nationwide database"), which

contains information about the quality of the soil. Management of a national database is

provided by the Ministry of agriculture ^ 3) through expert

the Organization, which on demand also provides summary information about the BPEJ and

their special purpose groups, for example. for an areal and qualitative protection

land and water, for regional planning, assessment of ecological stability

the landscape, creating economic instruments in agriculture and development

of the regions.



(2) to document the nationwide database they belong:



and BPEJ in digital) maps and graphical form



(b)) information reflecting the climate and soil conditions related to

code BPEJ,



(c) update BPEJ records),



(d) data on area representation) BPEJ in the cadastral territory of,



(e)) purpose of grouping BPEJ in the cadastral territory.



Update BPEJ



§ 3



(1) Update BPEJ (hereinafter referred to as "updates") is to detect changes of soil

and climate conditions agricultural land terrain exploration and

their evaluation against the conditions that characterize so far

set BPEJ, e.g. If there is a obvious and substantial changes in the

as a result of floods, landslide, significant degradation and destruction of the land

erosion, a fundamental change in the soil or in the hydromorfismu manifest

the earlier determination of the BPEJ, etc. Updates are validated and clarified, and the

define the new boundaries, different BPEJ, or change the code number

BPEJ. For the update also means finding data on the BPEJ parcels

where the BPEJ were not previously addressed. The reason for the update is also required

a complete and detailed national database. ^ 4) Updates under this

Ordinance changes are not affected during the BPEJ boundary inaccuracies of drawings

and correction of errors resulting from trapping of the maps. The update, which results in

the changed maps, land registry office provides BPEJ ^ 5) through

professional organizations that perform enters under a special prescription. ^ 6)



(2) the basis for the map update in digital or graphical

the form are:



and maps according to § 2), para. 2 (a). and in the scale of cadastral maps),



(b)), the land registry map



c) copies of maps at a scale of earlier land registration of cadastral maps

that are displayed as recorded in the land register plots

simplified the way. ^ 7)



(3) Land Office, found the reasons for the update within the meaning of

paragraph 1, and which took account of the requirements of the owners submitted

agricultural land, announce the opening and the range of updates, including

the term the implementation of field survey and its conditions, and the location where the

proposals for amendments of maps BPEJ and after their update has already changed the map BPEJ

landed to public inspection.



(4) the Land Office so requests, the municipality in whose territorial jurisdiction are

the land covered by the BPEJ update of the publication of the

the notification referred to in paragraph 3 in the place in the usual way and launched

BPEJ and update its scope separately inform the land registry office,

protection of agricultural land resources authority, ^ 8) tax office and the territorial

the Department of the Ministry of agriculture.



§ 4



(1) the authority shall ensure Land ^ 5) overhang design changes BPEJ (map to be displayed

on the průsvitce as the příložném material to map documents referred to in § 3

paragraph. 2 or as their trap) for 30 days for public

inspection. For this purpose, the authority shall request the community land, to the way in

the place of the usual inform the public of the place where it will be interpreted by design

changes to the maps, BPEJ and the period during which it will be possible to this proposal

take a peek, and the time limit within which everyone can apply to the design of the written

observations at the land Office. To later claimed the observations will not be

taken into account.



(2) Land Office after the evaluation of the observations received to the public makes the

based on the results of the update maps change BPEJ on the map of the substrate

referred to in § 3 (1). 2 (a). (b)), or (c)), where appropriate, on each map

documentation referred to in § 3 (1). 2 (a). (b)), and (c)) and shall indicate on the changed

maps BPEJ date of their validity, and thus update the BPEJ ends. About

stopping an update of BPEJ land authority shall inform the authorities of the

referred to in § 3 (1). 4 and also ask the municipality on the publication of a communication on the

stopping an update of BPEJ way in the usual place.



§ 5



The effectiveness of the



This Decree shall take effect on the date of publication.



Minister:



Ing. Fencl in r.



Č. 1



Characteristics of climatic regions

-------------------------------------------------------------------------------------------------------

Numeric Symbol characteristics of Average temperature Average Sum Probability Vlahova

the code of the regions regions above 10 C annual total annual dry security

regions of the temperature (C) precipitation in mm of the layers

period

as a percentage of

-------------------------------------------------------------------------------------------------------

0 VT very warm, 2800-3100 9-10 500-600 30-50 0-3

dry

-------------------------------------------------------------------------------------------------------

1 T 1 warm dry 2600-2800 8-500 40-60 0-2 9 <

-------------------------------------------------------------------------------------------------------

2 T 2 warm,

slightly dry 2600-2800 8-9 500-600 20-30 2-4

-------------------------------------------------------------------------------------------------------

3 T 3 warm,

slightly moist 2500-2800 (7) 8-9 550-650

(700) 10-20 4-7

-------------------------------------------------------------------------------------------------------

4 MT 1 slightly warm,

dry 2400-2600 7-8.5 450-550 30-40 0-4

-------------------------------------------------------------------------------------------------------

5 MT 2 slightly warm,

slightly moist 2200-2500 7-8 550-650

(700) 15-30 4-10

-------------------------------------------------------------------------------------------------------

6 MT 3 slightly warm

(to warm),

moist 2500-2700 7.5-8.5 700-9000-10 > 10

-------------------------------------------------------------------------------------------------------

7 MT 4 slightly warm,

moist 2200-2400 6-7 650-7505-15 > 10

-------------------------------------------------------------------------------------------------------

8 MCH slightly cool,

moist > 2000-2200 5-6 700-8000-5 10

-------------------------------------------------------------------------------------------------------

9 CH cool, moist under the 2000 > 0 800 10

------------------------------------------------------------------------------------------------------



Č. 2



Characteristics of the major soil units

01 Černozemě modal, černozemě carbonate, spraších or

the Carpathian flyši, land, moderate, without a skeleton, a very

deep, mostly with favorable water regime



02 Černozemě luvické on loess caps, moderate, without

the skeleton, mainly with favorable water regime




03 Černozemě černické, černozemě černické carbonate on the deep

spraších soil clays, marl or terraces, moderate,

bezskeletovité, with a regime favorable to slightly převlhčeným



04 Černozemě arenické at the sands or on shallow spraších

(maximum overlay up to 30 cm) stored on the sands

and štěrkopíscích, zrnitostně light, bezskeletovité, strongly

permeable soil with výsušným mode



05 Černozemě modal and černozemě modal carbonate, černozemě

luvické and fluvizemě modal and carbonate on spraších

with the power of 30 to 70 cm very permeable bedrock, medium

hard, mostly bezskeletovité, wizened, dependent on the

rainfall in growing period



06 Černozemě pelické and černozemě černické pelické on very heavy

substrates (clays, slínech, flyši and Carpathian tercierních

sediments), heavy to very heavy with vylehčeným orničním

Occasionally, like the horizon, with a tendency of the surface

převlhčení profile



07 Smonice smonice modal modal and carbonate, černozemě

pelické and černozemě černické pelické, always at very heavy

substrates, celoprofilově very hard, bezskeletovité, often

surface-periodic převlhčované



08 Černozemě modal and černozemě pelické, Brown, luvizemě,

where appropriate, the kambizemě luvické, where it is washed off cultivation

the transitional term or the substrate on the desktop is greater than 50%,

on the spraších, hlínách, svahových and loessial moderate

even more difficult, mostly without the skeleton and of a higher hostile



09 Šedozemě modal including oglejených and faintly šedozemě luvické on

spraších, moderate bezskeletovité, favourable, vláhovými

ratios



10 Brown modal including oglejených on spraších weakly, medium

heavy with slightly heavier lowlifes without the skeleton, with favorable

vláhovými ratios to drier



11 Brown modal including oglejených on weakly loess

and soliflukčních hlínách (prachovicích), a moderate with a heavier

the low life, without a skeleton, with favourable humidity conditions



12 Brown modal, modal and kambizemě kambizemě luvické,

all including oglejených forms of weakly on svahových

(polygenetických) hlínách, moderate to severe low life

medium-skeletovité, vododržné, in the brain with the local

převlhčením



13 Brown Brown luvické, modal, modal, luvizemě

fluvizemě modal and stratified, on eolických substrates,

where appropriate, the svahovinách (polygenetických hlínách) with the powers

a maximum of 50 cm is stored on very permeable medium,

bezskeletovité-to-skeletovité, dependent on rain

rainfall in growing period



14 Luvizemě modal, Brown luvické including oglejených on weakly

loess hlínách (prachovicích) or svahových

(polygenetických) hlínách with a strong admixture of eolickou, medium

difficult with severe lowlifes, with ratios of favourable vláhovými



15 Luvizemě modal and Brown luvické, including oglejených varieties

the svahových hlínách with eolickou admixture, moderate to

heavy to moderate skeletovité, favourable vláhově only

short převlhčením



16 Luvizemě modal and Brown arenické, or possibly even slightly

oglejené on light to zahliněných terraces, sandstone

and Sandy loess štěrkopíscích with overlay and prachovic

in the power 30 to 60 cm, zrnitostně moderate lighter until

slightly skeletovité, vláhově less favourable to unfavourable



17 Luvizemě arenické i oglejené, slightly on light, permeable

substrates, wizened, dependent on rainfall or závlaze



18 Rendziny, rendziny kambické and modal rendziny extracted to

limestone and travertinech, moderate to heavy, slightly lighter

to moderate skeletovité, less vododržné



19 Pararendziny modal, kambické and extracted the opukách

and hard slínovcích or calcareous svahových hlínách, medium

to severe, slightly to moderately skeletovité, with a good vláhovým

mode to short-převlhčené



20 Pelozemě modal, bleached and melanické, regozemě pelické,

kambizemě pelické i pararendziny pelické, always at very heavy

substrates, clays, slínech, flyši, tercierních sediments

and similarly, the soil with a small vodopropustností, mostly without the skeleton,

But even moderate skeletovité, often slightly oglejené



21 the land arenického, regozemě, pararendziny subtype, kambizemě,

or even fluvizemě on light, nevododržných, strongly

výsušných substrates



22 Land as the preceding HPJ 21 on slightly heavier substrates

the type of aluminium sand or sandy clay with water regime somewhat

more favourable than the previous



23 Regozemě arenické and kambizemě arenické, in both cases

I weakly oglejené on zahliněných sands and štěrkopíscích or

the terraces on the impermeable bedrock clays, marl, districts

and tercierních clays, water regime is very unstable, and it always

Depending on the depth of the impermeable layer and the powers of the overlap



24 Kambizemě eubazické to mezobazické and modal kambizemě pelické

from the svahovin karbonátosilikátových rock relocated-districts

and the kulmských shale, moderate to severe to moderate

skeletovité, vododržností



25 Kambizemě modal and bleached, eubazické to mezobazické,

even kambizemě pelické to the opukách and hard slínovcích,

medium-heavy flyši, permokarbonu, moderate, to moderate

skeletovité, soil with good water capacity



26 Kambizemě eubazické and mezobazické on the modal-schist,

mostly moderate, to skeletovité, with favorable

vláhovými conditions



27 Kambizemě eubazické up mezobazické on the modal sandstones,

drobách, curling iron, brdském, flyši, zrnitostně Cambrian light or

moderate lighter, with different soil skeletovitostí, wizened



28 Kambizemě eubazické kambizemě modal, modal eutrophic on

basis and ultrabazických rocks and their tufech, mostly

moderate, without a skeleton to moderate skeletovité, with favorable

humidity conditions, medium deep



29 Kambizemě eubazické mezobazické including modal to weakly

oglejených varieties, dug, svorech, fylitech, or

žulách, moderate to moderate lighter, without a skeleton to

medium-skeletovité, with the prevailing good vláhovými conditions



30 Kambizemě eubazické to mezobazické to svahovinách

sedimentary rocks-sandstone, permokarbon, flyš, medium

hard to lighter, to moderate skeletovité, favourable to vláhově drier



31 Kambizemě arenické, eubazické the modal up to mezobazické on

sedimentary, minerálně poor substrates-sandstone

Chalk slate, permokarbon, however there is always light, without a skeleton to

medium-skeletovité, little vododržné, wizened



32 Kambizemě eubazické up mezobazické on the modal gross

zvětralinách, permeable, minerálně poor substrates,

žulách, syenitech, granodioritech, less ortorulách, medium

heavy lighter with a higher content of grusu, vláhově more favorable in

wetter climate



33 Kambizemě eubazické to mezobazické and modal kambizemě modal

rubifikované on zvětralinách permokarbonu, heavy heavy

even moderate, sometimes even moderate skeletovité, favourable

vláhovými conditions



34 Kambizemě dystrické, kambizemě modal mezobazické

I kryptopodzoly the žulách, modal dug, svorech and fylitech,

moderate lighter to medium skeletovité, vláhově stocked,

However, in a slightly cold climate region



35 Kambizemě dystrické, kambizemě mezobazické, modal

kryptopodzoly modal including weakly oglejených varieties, on

schist, permokarbonu, flyši, neutral igneous

rocks and their svahovinách, moderate, to moderate

skeletovité, vláhově to převlhčené, slightly favourable in a slightly

cold climate region



36 Kryptopodzoly modal, modal podzol, kambizemě dystrické,

possibly kambizem modal mezobazická, without distinction

Mother rocks, mostly moderate lighter, with varying

skeletovitostí, soil to slightly převlhčované, but always

in cold climate region



37 Kambizemě rock, kambizemě, kambizemě rankerové modal

and rankery modal on hard substrates without distinction,

in podorničí from 30 cm strongly skeletovité or fixed-rock,

weak to moderate skeletovité, in the ornici moderate lighter to

light, mainly dependent on rainfall, wizened



38 of the soil as the previous 37, however, the zrnitostně HPJ moderate

to severe, due to the composition of the zrnitostnímu with a vododržností



39 Litozemě modal on substrates without a resolution, with shallow drnovým

the horizon with outcrops of solid rocks, usually 10 to 15 cm

powerful, with unfavourable vláhovými conditions



40 Soil with sklonitostí greater than 12 degrees, kambizemě, rendziny,

pararendziny, rankery, regozemě, černozemě, Brown and others,

zrnitostně moderate lighter to light, with varying

skeletovitostí, vláhově dependent on the climate and exposure



41 as for the HPJ 40 but zrnitostně moderate to very


heavy with somewhat more favorable vláhovými ratios



42 oglejené on loess hlínách Brown (prachovicích),

spraších, moderate, without a skeleton, with a tendency to temporarily

převlhčení



43 Brown luvické, luvizemě oglejené on loess hlínách

(prachovicích), a moderate, in the brain even harder without skeleton

or just with the addition, are prone to převlhčení



44 Pseudogleje pseudogleje luvické, modal, on loess hlínách

(prachovicích), medium hard, harder in the brain, without the skeleton

or blended with, are prone to temporary waterlogging



45 Brown oglejené on svahových (polygenetických) hlínách,

often with eolickou admixture, moderate, without a skeleton to slightly

skeletovité, are prone to temporary waterlogging



46 luvické oglejené Brown luvizemě oglejené on the svahových,

(polygenetických) hlínách, moderate in brain harder, without

the skeleton to moderate skeletovité, with a tendency to temporarily

waterlogging



47 Pseudogleje pseudogleje luvické, modal, kambizemě oglejené on

svahových (polygenetických), moderate hlínách, in dregs

harder-to-skeletovité, are prone to temporary waterlogging



48 Kambizemě oglejené, rendziny kambické oglejené, pararendziny

kambické oglejené and pseudogleje opukách, modal on the slates,

permokarbonu or flyši, moderate lighter to moderate,

without the skeleton to moderate skeletovité, with a tendency to temporarily,

mostly spring gun



49 Kambizemě pelické oglejené, rendziny pelické oglejené,

pararendziny kambické and pelické oglejené and pelozemě oglejené on

Clay Shales, permokarbonu and zvětralinách districts, tufech

and basic, zrnitostně, severe to very severe to

medium-skeletovité, with a higher tendency to temporary waterlogging



50 Kambizemě oglejené and pseudogleje žulách, modal on the dug out

and other hard rocks (that are not in the HPJ 48,49), medium

heavy lighter to moderate, slightly to moderately skeletovité,

prone to temporary waterlogging



51 Kambizemě oglejené and pseudoglej zahliněných the modal

štěrkopíscích, terraces and nature, zrnitostně light or

moderate lighter, without a skeleton to moderate skeletovité,

with an irregular water regime dependent on rainfall



52 Pseudogleje modal, kambizemě oglejené on lighter sediments

limnického tercieru (freshwater upper Cretaceous and tercierní

the Danube), often with the addition of eolického material, as a rule, only

slightly skeletovité, zrnitostně moderate lighter to light,

prone to temporary převlhčení



53 Pseudogleje pelické planické, kambizemě oglejené on heavier

limnického tercieru (freshwater sediments of the upper Cretaceous

and tercierní of the Danube), moderate to severe, rarely

medium-skeletovité, low permeable, periodically waterlogged



54 Pseudogleje pelické, pelozemě oglejené, pelozemě bleached

oglejené, kambizemě pelické oglejené, pararendziny pelické

oglejené on slínech, and neogenu districts of the marine clays

and the clay sediments of the limnického tercieru (freshwater

upper Cretaceous and tercierní of the Danube), hard to very hard,

with very adverse physical characteristics



55 Fluvizemě psefitické, arenické stratified, černice arenické

I pararendziny arenické on the uloženinách floodplain, often light

with bedrock terraces, usually sandy, wizened



56 Fluvizemě eubazické up mezobazické, modal fluvizemě kambické,

koluvizemě modal on the alluvial soil-uloženinách, often

terraces, moderate lighter to moderate, usually without

the skeleton, vláhově beneficial



57 Fluvizemě pelické and kambické eubazické to mezobazické to

heavy alluvial uloženinách, to very difficult, without the skeleton,

favourable humidity ratios up to převlhčení



58 Fluvizemě glejové on the uloženinách floodplain, or soil-

terraces, moderate or moderate lighter, only weakly

skeletovité, 1 m below the water level, the establishment of conditions after drainage

a favourable



59 Fluvizemě glejové on the uloženinách floodplain, hard and very hard

without the skeleton, the establishment of the adverse conditions, require the regulation of

the water regime



60 Černice and modal modal černice carbonate and černice

arenické on uloženinách, no Graben village ... and floodplain loess hlínách,

moderate, without a skeleton, favorable to the establishment to slightly

wetter



61 Černice and pelické pelické carbonate on floodplain černice.

uloženinách, hlínách, spraších, loess clays and slínech,

hard and very hard, without a skeleton, a tendency to převlhčení



62 Černice glejové, černice glejové carbonate on the floodplain

uloženinách, no Graben village ... as well as loess hlínách, moderate

even lighter, without a skeleton, waterlogged bottom water temporarily varying

at a depth of 0.5-1 m



63 pelické glejové and carbonate Černice on floodplain uloženinách,

clays and slínech, heavy and very heavy, with no skeleton, adverse

the establishment of ratios as a result of high levels of ground water



64 Gleje modal, modal and stagnogleje fluvické on gleje

svahových hlínách, uloženinách, clay, and alluvial slínitých

materials, zkulturněné, with a modified aquatic mode, medium

hard to very hard, without a skeleton or slightly skeletovité



65 Gleje akvické, histické, modal boggy in some parts, organozemě

glejové uloženinách, svahovinách on the floodplain, rocks

tercieru and districts limnického, mild to very severe with a higher

the content of organic matter, and wetter than HPJ 64



66 Stagnogleje modal and histické on the sands, clays, slínech

and floodplain uloženinách, mild to very severe with a higher content of

organic substances, very negative water regime, unsuitable for

his editing



67 Gleje modal on different substrates often vrstevnatě

stored in positions of broad depression and Planar units,

moderate to severe, when rivers depend on the height of

blood flow, flooded, it's hard to odvodnitelné



68 Gleje modal modal boggy in some parts, gleje histické, černice

glejové uloženinách on the floodplain in the boggy in some parts around smaller

water flows, soil narrow depression including slopes, difficult to

identifiable, moderate to very severe, adverse water

mode



69 Gleje akvické, gleje akvické zrašeliněné and gleje histické on

floodplain uloženinách or svahovinách, mostly heavy, significantly

waterlogged soil, depression and Planar complexes



70 Gleje, gleje fluvické and modal fluvizemě glejové on the floodplain

uloženinách, where appropriate, with bedrock terraces, while the terrace sections

wide plains, moderate to very heavy, at elevated level

the water in the flow are suffering from flooding



71 Gleje fluvické, fluvizemě glejové, with the same characteristics as .HPJ

70, but significantly wetter in terraced sections of narrow niv



72 Gleje fluvické gleje fluvické histické and boggy in some parts of the floodplain

uloženinách, moderate to very heavy, permanently under the influence of

the water level in the flow



73 Kambizemě oglejené, pseudogleje glejové i hydroeluviální, gleje

hydroeluviální and surface, located in svahových

positions, normally the waterlogged areas, with the occurrence of svahových

moderate to very heavy to medium skeletovité



74 Pseudogleje glejové i hydroeluviální, gleje surface

boggy in some parts and gleje surface histické, gleje akvické,

stagnoglej modal, soils of moderate to very severe, up to

medium skeletovité located in svahových positions,

waterlogged, svahovými Springs, often boggy in some parts



75 Kambizemě oglejené, kambizemě glejové, pseudogleje i gleje,

the soil of the lower parts of the slopes, the gun more prominent than the 74, HPJ

difficult-to-define the transitions on the deluviích rocks

and svahovinách, to skeletovité



76 Pseudogleje, gleje i histické, organozemě boggy in some parts, always

with a strong rašeliněním and zamokřením, with difficult accessibility,

as a rule, moderate to very heavy, skeletovité



77 Shallow ravine to a depth of 3 m with the occurrence of koluvizemí, regozemí,

kambizemí, and more, with carve in realistic erosion smyvy ornic, different grain size,

bezskeletovité to heavily skeletovité, for agricultural use

a few appropriate



78 more than 3 m Deep ravine, with a nemapovatelným representation

hydromorfních soil-glejů, pseudo-glejů and koluvizemí all

subtypes with a significantly adverse humidity conditions, for

Agriculture is inappropriate.



Č. 3



Characteristics of hostile and exposure



Sklonitost

+---------------------------------------------------------+

| Characteristics Of The Category Code |

+---------------------------------------------------------+

|-0 0 1st. the full plane |

|-1 1 3rd. plane |

|-7 2 3rd. a slight slope |

|-12nd 3 7. central tendency |

|-17 4 12nd. a significant slope |

| 5 17-25th. steep slope |

| 6 25th. Cliff |

+---------------------------------------------------------+



Exposure



The territory of the BPEJ against the dvep reflects the world in four categories

marked with the codes 0-3.

+------------------------------------------------------------------+

| The Code Characteristics |

+------------------------------------------------------------------+


the všesměrnou exposure | 0 |

| 1 South (southwest to Southeast) |

| 2 East and West (southwest to Northwest, jihovýhod to |

| Northeast) |

North (Northwest | 3-Northeast |

+------------------------------------------------------------------+



In the climatic regions (according to annex No 1) in the case of numeric codes 0, 1, 2,

3, 4 and 5 shall be considered as a negative exposure South, the other exposure

consider as equal.



In the climatic regions (according to annex No 1) in the code numbers 6, 7, 8

and 9 shall be considered as a negative exposure North and East-West exposure

and the South are discounted as equal.



Fourth digit BPEJ is a combination of hostile and

exposure is encoded as follows:

+--------------------------------------------------------------+

Numeric code code hostile | Code exposure |

+--------------------------------------------------------------+

|0 0 - 1 0 |

|1 2 0 |

|2 2 1 |

|3 2 3 |

|4 3 1 |

|5 3 3 |

|6 4 1 |

|7 4 3 |

|8 5 - 6 1 |

|9 5 - 6 3 |

+--------------------------------------------------------------+



Č. 4



Characteristics of skeletovitosti and depth of soil



Skeletovitost

+------------------------------------------------------------------------------------+

| The Code Characteristics |

+------------------------------------------------------------------------------------+

| bezskeletovitá mixed with a 0 with a total content of the skeleton to 10% |

skeletovitá with weakly | 1 total 10-25% of the skeleton |

| skeletovitá with 2 medium total skeleton 25-50% |

strongly skeletovitá with | 3 total skeleton nad50% |

+------------------------------------------------------------------------------------+



The contents of the skeleton is expressed as total volume of gravel (solid content

particles of rocks from 4 to 30 mm) and stone (solid particles of rocks over 30

mm).



The depth of soil



It expresses the depth part of the soil profile either solid rock limited

or a strong skeletovitostí.

+------------------------------------------------------------------+

| The Code Characteristics |

+------------------------------------------------------------------+

> | 0 60 cm soil deep |

| 1 30-60 cm soil medium deep |

| 2 < 30 cm shallow soil |

+------------------------------------------------------------------+



The fifth digit is preceded by a combination of skeletovitosti and

the depth of the land as follows:

+-------+--------------+----------------------------+----------+------------------------------------+

| Number | Code | Characteristics of code | Code | Characteristics of soil depth |

| code | skeletovitosti | skeletovitosti | depth | |

| | | | soil | |

+-------+--------------+----------------------------+----------+------------------------------------+

|0 | 0 | bezskeletovitá, additive | 0 | deep |

|1 | 0 - 1 | bezskeletovitá, additive, | 0-1 | deep, moderately deep |

| | | weakly skeletovitá | | |

|2 | 1 | weakly skeletovitá | 0 | deep |

|3 | 2 | medium-skeletovitá | 0 | deep |

|4 | 2 | medium-skeletovitá | 0-1 | deep, moderately deep |

|5 | 1 | weakly skeletovitá | 2 | shallow |

|6 | 2 | medium-skeletovitá | 2 | shallow |

|7+) | 0 - 1 | bezskeletovitá, additive, | 0-1 | deep, moderately deep |

| | | weakly skeletovitá | | |

|8+) | 2 - 3 | medium skeletovitá, | 0-2 | deep, moderately deep, shallow |

| | | strongly skeletovitá | | |

|9+) | 0 - 3 | bezskeletovitá, additive, | 0-2 | deep, moderately deep, shallow |

| | | slightly skeletovitá, | | |

| | | medium skeletovitá, | | |

| | | strongly skeletovitá | | |

+-------+--------------+----------------------------+----------+------------------------------------+



+) Applies only to land on the hostile > 12 St. i.e. HPJ 40, 41

and for the HPJ 39 infants (rankerových) soils.



§ 8 paragraph 1). 8 of the law No. 284/1991 Coll., on land and

land offices, as amended by Act No. 38/1993 Coll. and Act No.

217/1997 Sb.



2) section 13 (a). (d)) and section 11 (b). (b) Act No. 284/1991) Sb.



3) section 31 of Act No. 576/1990 Coll., on rules of management of the budget

means the United States and municipalities in the Czech Republic (budget

the rules of the Republic), as amended.



4) Eg. section 15 of Act No. 334/1992 Coll., on the protection of agricultural land

the Fund, as amended by Act No. 10/1993 Coll. and section 15 para. 5 of Decree No.

13/1994 Coll. laying some of the details of the protection

agricultural land resources.



5) section 11 of the Act on land and land offices.



6) Act 513/1991 Coll., the commercial code, as amended

regulations.



7) § 28 para. 3 of Act No. 344/1992 Coll., on the real estate of the Czech

Republic (Act), as amended by Act No. 89/1996 Coll.



8) Act 334/1992 Coll., as amended.