546/2002 Sb.
DECREE
of 12 October. December 2002,
amending Decree No 327/1998 Coll., laying down the
characteristics of soil environmental bonitovaných of the units and the procedure for
their management and update
The Ministry of agriculture lays down, pursuant to section 8 (2). 8 of Act No. 283/1991
Coll., on land and land offices, as amended by Act No.
217/1997:
Article. (I)
Decree No. 327/1998 Coll., laying down the characteristics of the
bonitovaných soil-ecological units and the procedure for their guidance and
Update, is amended as follows:
1. In article 3, paragraph 3. 1 the words "District Land Office (hereinafter referred to as" land
the Office ") ^ 5)" shall be replaced by the words "land úřad5)".
Footnote. ^ 5) is added:
5) section 11 of the Act on land and land authorities. ".
2. in annex No 1, in the heading of the first column, the word "Code" is replaced by
the words "code number" and at the end of the title of the seventh column, Word
the "period", the words "percentage".
3. Appendix 2 is added:
"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 (maximum spraších
the overlay up to 30 cm) stored on the sands and štěrkopíscích, zrnitostně
light, bezskeletovité, highly permeable soils 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,
medium 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 horizon,
Occasionally, like with a tendency of surface převlhčení in the profile
07 Smonice smonice modal modal and carbonate, pelické, and černozemě
černozemě černické pelické, always at very difficult 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 an area bigger than 50%, to
spraších, hlínách, svahových and loessial moderate even harder,
mostly without the skeleton and of a higher hostile
09 Šedozemě modal including oglejených and faintly šedozemě luvické on
spraších, moderate, bezskeletovité, vláhovými, with favourable conditions
10 Brown modal including oglejených on spraších weakly, moderate
with a slightly heavier for the low life, without a skeleton, with favourable ratios of up to vláhovými
drier
11 Brown modal including oglejených on the loess and weakly
soliflukčních hlínách (prachovicích), a moderate with a heavier lowlifes,
without the skeleton, with favourable humidity conditions
12 Brown kambizemě modal, modal and kambizemě luvické, all
including the oglejených forms of the weakly svahových (polygenetických) hlínách,
moderate to severe lowlifes, to medium-skeletovité, vododržné,
base with local převlhčením
13 Brown Brown, modal, modal, luvické luvizemě fluvizemě
modal and stratified, on eolických substrates, where appropriate, the
svahovinách (polygenetických hlínách) with powers up to 50 cm
stored on very permeable medium, to medium-bezskeletovité
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 with severe, moderate, lowlifes, with
vláhovými ratios of favourable
15 Luvizemě modal and Brown luvické, including oglejených varieties to
svahových hlínách with eolickou admixture, moderate to severe, up to
moderate skeletovité, favourable with only short vláhově převlhčením
16 Luvizemě modal and Brown arenické, or possibly even weakly oglejené
on light to zahliněných terraces, sandstones and štěrkopíscích with
overlay Sandy loess and prachovic in power 30 to 60 cm,
zrnitostně moderate to slightly lighter, 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
medium-skeletovité, less vododržné
19 Pararendziny modal, kambické and extracted the opukách and hard
svahových hlínách slínovcích or calcareous, moderate to severe,
a weakly to moderately skeletovité, with a good vláhovým to short term mode
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 the like,
soil with a small vodopropustností, mostly without the skeleton, but also 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 media type
aluminium sand or sandy clay with water regime somewhat more favourable
than the previous
23 Regozemě arenické and kambizemě arenické, in both cases, even weakly
oglejené on štěrkopíscích or zahliněných sands and terraces, located
the impermeable bedrock clays, marl, and tercierních districts of clays, water
the scheme is highly unstable, always depending on the depth of impermeable
layer and the powers of the overlap
24 Kambizemě eubazické to mezobazické and modal kambizemě pelické from
svahovin karbonátosilikátových rock relocated-kulmských districts
shale, moderate to severe to moderate skeletovité, medium
vododržností
25 Kambizemě modal and bleached, eubazické to mezobazické,
I kambizemě pelické on slínovcích opukách and hard, medium-hard
flyši, permokarbonu, moderate, to medium skeletovité, the soil with
good water capacity
26 Kambizemě eubazické and mezobazické on the modal-schist, mostly
moderate, to moderate skeletovité, favourable ratios with vláhovými
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 the basis
and ultrabazických rocks and their tufech, mostly moderate, without
the skeleton to moderate skeletovité, favourable humidity conditions, with
medium deep
29 Kambizemě eubazické to mezobazické including modal weakly oglejených
varieties, dug, svorech, fylitech, or žulách, moderate
to moderate lighter, without a skeleton to moderate skeletovité, with
prevailing good vláhovými conditions
30 Kambizemě eubazické up mezobazické on svahovinách sedimentary
rocks-sandstone, permokarbon, flyš, moderate lighter, to moderate
skeletovité, vláhově favorable to the drier
31 Kambizemě arenické, eubazické the modal up to mezobazické on
sedimentary, minerálně poor substrates-sandstone, the Cretaceous
Slate, permokarbon, however there is always light, without a skeleton to medium
skeletovité, little vododržné, wizened
32 Kambizemě eubazické up mezobazické on the modal raw zvětralinách,
permeable, minerálně poor substrates, žulách, syenitech,
granodioritech, less ortorulách, moderate lighter with a higher content of
grusu, vláhově more favorable in the wetter climate
33 Kambizemě eubazické to mezobazické and modal kambizemě modal
rubifikované zvětralinách permokarbonu, in heavy and medium
heavy, sometimes even moderate skeletovité, favourable vláhovými ratios
34 Kambizemě dystrické, kambizemě mezobazické and kryptopodzoly modal
modal on the žulách, fylitech, svorech and dug, moderate lighter to
medium skeletovité, vláhově stocked, but always in a slightly cool
the climate of the region
35 Kambizemě dystrické, kambizemě mezobazické, kryptopodzoly modal
modal including weakly oglejených varieties, on shale, permokarbonu,
flyši igneous rocks, neutral and their svahovinách, medium
heavy to moderate skeletovité, favourable to slightly vláhově převlhčené, in
slightly cool climate region
36 Kryptopodzoly modal, modal podzol, kambizemě dystrické,
possibly kambizem modal mezobazická, without resolution of the mother
rocks, mostly moderate lighter, with different skeletovitostí, the soil to
slightly převlhčované, but always in a cool climate region
37 Kambizemě rock, kambizemě, rankerové and modal kambizemě rankery
modal on hard substrates without distinction, in podorničí from 30 cm
strongly skeletovité or fixed-rock, slightly to moderately skeletovité,
in the ornici moderate lighter to light, predominantly wizened, dependent on the
precipitation
38 of the soil as the previous 37, however, HPJ zrnitostně moderate to
difficult, 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, with a powerful
adverse 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 the 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 with
additives, are prone to temporary waterlogging
45 Brown oglejené on svahových (polygenetických) hlínách, often with
eolickou, additive moderate, without a skeleton to slightly skeletovité,
prone to temporary waterlogging
46 luvické oglejené Brown luvizemě oglejené on the svahových,
(polygenetických) hlínách, moderate in brain harder without skeleton
to moderate skeletovité, are prone to temporary waterlogging
47 Pseudogleje pseudogleje luvické, modal, kambizemě oglejené on
svahových (polygenetických), moderate hlínách, in straight-up harder
medium-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, mainly
spring gun
49 Kambizemě pelické oglejené, rendziny pelické oglejené, pararendziny
kambické and pelické oglejené and pelozemě oglejené on clay
zvětralinách shale, permokarbonu and tufech districts, and basic
, zrnitostně, severe to very severe to moderate skeletovité, with
more prone to temporary waterlogging
50 Kambizemě oglejené and pseudogleje žulách, dug out the modal and other
hard rocks (that are not in the HPJ 48,49), moderate lighter to
moderate, slightly to moderately skeletovité, with a tendency to temporarily
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
mode dependent on rainfall
52 Pseudogleje modal, kambizemě oglejené on lighter sediments
limnického tercieru (freshwater upper Cretaceous and tercierní of the Danube),
often blended with eolického material, as a rule, only slightly skeletovité,
zrnitostně moderate lighter to light, with a tendency to temporarily
převlhčení
53 Pseudogleje pelické planické, kambizemě oglejené on heavier
the sediments of the upper Cretaceous limnického tercieru (freshwater and tercierní
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, marine clays and neogenu districts and clay sediments
limnického tercieru (freshwater upper Cretaceous and tercierní of the Danube),
heavy to very heavy, with very adverse physical characteristics
55 Fluvizemě psefitické, arenické, arenické and stratified černice
pararendziny arenické light uloženinách on the floodplain, often with a subsoil
terraces, usually sandy, wizened
56 Fluvizemě eubazické up mezobazické, modal fluvizemě kambické,
koluvizemě modal on the floodplain uloženinách, often with bedrock terraces,
moderate lighter to moderate, usually without the skeleton, vláhově
a favourable
57 Fluvizemě pelické and kambické eubazické to mezobazické on heavy
uloženinách floodplain, up to very hard, without a skeleton, favourable humidity
ratios up to převlhčení
58 Fluvizemě glejové on the uloženinách floodplain, or soil-
terraces, moderate or moderate lighter, only slightly skeletovité,
1 m below the water level, the establishment of ratios of favourable after drainage
59 Fluvizemě glejové on the uloženinách floodplain, heavy and very difficult, without
the skeleton, the establishment of the adverse conditions, require the regulation of the water regime
60 Černice and modal modal černice carbonate and arenické in černice.
uloženinách floodplain, no Graben village ... as well as loess hlínách, moderate, without
the skeleton, the establishment of conditions conducive to slightly wetter
61 Černice and pelické pelické carbonate on floodplain černice.
uloženinách, hlínách, spraších, loess clays and slínech, heavy and
very hard, without a skeleton, a tendency to převlhčení
62 Černice glejové, černice glejové carbonate on floodplain uloženinách,
No Graben village ... as well as loess hlínách, moderate and lighter, without a skeleton,
waterlogged bottom water temporarily, varying in 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, the adverse conditions the establishment
as a result of high levels of ground water
64 Gleje modal, modal and stagnogleje gleje fluvické on svahových
hlínách, uloženinách, alluvial clay and slínitých materials
zkulturněné, with a modified water regime of moderate to very severe,
without the skeleton or slightly skeletovité
65 Gleje akvické, histické, organozemě, glejové modal boggy in some parts of the
floodplain uloženinách, svahovinách, tercieru and limnického rocks
districts, mild to very severe with a higher content of organic substances, wetter
than HPJ 64
66 Stagnogleje modal and histické on the sands, clays, and floodplain slínech
uloženinách, mild to very severe with a higher content of organic substances
very unfavourable water regime, unsuitable for its adjustment
67 Gleje modal on different substrates often stored in vrstevnatě
positions of broad depression and Planar complexes, moderate to severe,
When rivers flow levels dependent on height, flooded, hard to
odvodnitelné
68 Gleje modal modal boggy in some parts, gleje histické, černice glejové
boggy in some parts of the floodplain uloženinách around the smaller water flows, soil
the narrow depression including slopes, difficult-to-define, moderate to
very difficult, negative water balance
69 Gleje akvické, gleje akvické zrašeliněné and gleje histické in the floodplain
uloženinách or svahovinách, mostly heavy, a waterlogged soil, significantly
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, the surface of the water in the
flow suffers from flooding
71 Gleje fluvické, fluvizemě glejové, with the same characteristics as the 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 levels of
the water in the flow
73 Kambizemě oglejené, pseudogleje glejové i hydroeluviální, gleje
hydroeluviální and surface, located in svahových positions,
as a rule, waterlogged areas of svahových, with the appearance of moderate to
very hard to moderate skeletovité
74 Pseudogleje glejové i hydroeluviální, gleje surface boggy in some parts and
gleje surface histické, gleje akvické, stagnoglej modal, soil
moderate to very heavy to medium skeletovité is located in the
svahových positions, waterlogged, svahovými Springs, often boggy in some parts
75 Kambizemě oglejené, kambizemě glejové, pseudogleje i gleje, soil
the lower parts of the slopes, the gun more prominent than the HPJ 74, difficult to
-define the transitions on the deluviích rocks and svahovinách, to moderate
skeletovité
76 Pseudogleje, gleje i histické, organozemě boggy in some parts, always with the
pronounced 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, suitable for the agricultural use of little
78 more than 3 m Deep ravine, with a nemapovatelným representation
hydromorfních soil-glejů, pseudo-glejů and koluvizemí all subtypes with
significantly adverse humidity ratios for agriculture unsuitable. ".
4. Appendix 3:
"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) for numeric
codes 0, 1, 2, 3, 4 and 5 shall be considered as negative, southern exposure
other exposure are discounted as equal.
In the climatic regions (according to annex No 1) in the case of numeric codes 6
7, 8 and 9 shall be considered as a negative exposure North and exposure
the East-West and South are discounted as equal.
Fourth digit BPEJ is a combination of hostile
and the 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 ". |
+--------------------------------------------------------------+
5. Appendix 4:
"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 skeleton 10-25% |
| 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 containing gravel
(particles of rocks from 4 to 30 mm) and stone (solid particles
rocks over 30 mm).
The depth of soil
It expresses the depth part of the soil profile limited either fixed
rock or 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
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. ".
Article II
This Decree shall enter into force on 1 January 2000. January 1, 2003.
Minister:
Ing. Palas in r.
