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.