Decree No. 227 / 2018 Coll.
Ordonnance on the characterisation and management and updating of the soil units
Valid
Effective from 01.01.2019
227
DECLARATION
of 4 October 2018
on the characteristics and procedures for the management and updating of soil-based environmental units
The Ministry of Agriculture provides pursuant to Article 8 (4) of Act No. 139 / 2002 Coll., on Land Adjustments and Land Offices and amending Act No. 229 / 1991 Coll., on the Treatment of Property Relations with Land and Other Agricultural Property, as amended, as amended, as amended by Act No. 503 / 2012 Coll. and Act No. 295 / 2017 Coll.:
Subject matter
This decree regulates the characteristics of the soil-ecological units and the procedure for their management and updating.
Characterisation of soil-protected ecological units
The protected soil-ecological unit (1) is characterised by the climate region, the main soil unit, the inclination and exposure to the world parties, the skeletons and the depth of the soil, specifying the main soil and climatic conditions of the land under assessment;
(a) the climate region comprises areas with approximately the same climate conditions for the growth and development of agricultural crops as set out in Annex 1 to this Regulation; is expressed as the first digit of the five-digit code,
(b) the main soil unit is a special-purpose grouping of soil forms of related properties as set out in Annex 2 to this Decree; is expressed in the second and third digits of the five-digit code,
(c) the inclination and exposure to the parties to the world shall reflect the shape of the surface of the agricultural parcel in accordance with Annex 3 to this Decree; are expressed in the fourth digit of the five-digit code resulting from their combination; and
(d) the skeleton, which is the combination of the gravel and stone content of the ornice and the gravel and stone content of the bottom not exceeding 0,6 m, and the depth of the soil referred to in Annex 4 to this Decree, are expressed by the fifth digit of the five-digit code resulting from their combination.
Management of Bonized Soil Organic Units
(1) Bound soil ecological units are uniformly managed in the national database of Bound soil ecological unit (2). The five-digit code of the Bonized Soil Organic Units is available in the Real Estate Register.
(2) The documentation of the national database of soil-protected organic units belongs to:
(a) maps of Bonized Soil Organic Units in digital raster form; and
(b) records of the update of the Bonified Soil Organic Units - the Bonitation Information System.
Update of Bonized Soil Organic Units
(1) The update of the Bonized Soil Organic Units shall identify and evaluate changes in soil and climatic conditions of agricultural parcels by field survey compared to those characterised by the previously established Soil Bonified Organic Unit, in particular where there have been apparent and substantial changes due to flood, landslide, significant degradation and destruction of soil erosion, a major change in hydromorphism of the Soil, or where previously the Bonified Soil Organic Units have been clearly misdetermined.
(2) The update of the Bonified Soil Organic Units shall verify and specify, thereby defining, the boundaries of the different Soil Bonified Organic Units or, where appropriate, the code number of the Bonified Soil Organic Units.
(3) When updating Bonized Soil Organic Units, it is performed
(a) updating the soil-protected ecological units of the entire cadastral territory or parts of the cadastral territory, where appropriate;
(b) a follow-up by supplementing and specifying national databases of granulated soil and ecological units (3) and the determination of bonized soil units on newly born agricultural parcels where they have not previously been identified; and
(c) updating the protected soil-ecological units to a part of the cadastral territory.
(4) No changes in the course of the borders of the bonized soil-based units affected by the inaccuracy of the schematics and correction of errors arising from the map printing shall be made when updating the soil-based units.
(5) As a result of the update of the Bonized Soil Organic Units, the amended maps of the Soil Organic Units are modified.
(1) The map supporting the update of the bonized soil ecological units in digital or analogue form, where appropriate, is:
(a) the maps referred to in Article 3 (2) (a);
(b) cadastral maps; and
(c) copies of maps of earlier land records on the scale of the cadastral map showing parcels registered in the cadastral by simplified means (4).
(2) The Land Authority, if it has found reasons for updating the chartered soil ecological units, shall notify the opening and scope of the update, including the date of implementation of the field survey and its conditions, and the place where the proposals for modified maps of the charred soil ecological units will be unloaded for public consultation.
(3) The Land Office shall separately inform the locally competent cadastral office, the authority for the protection of the agricultural land fund of the municipality's enlarged office and the tax office of the bonized soil units of the start of the update.
(4) The Land Authority shall ensure that the proposals for amended maps of soil-protected organic units are unloaded for 30 days for public consultation.
(5) Within 2 months of the expiry of the deadline for the landing of the amended maps of the soil-protected organic units, the Land Office shall evaluate the comments to the public and, where appropriate, draw up the amended maps of the soil-protected organic units on the map referred to in Article 5 (1) (b).
(6) The Land Authority shall, within 3 months of the preparation of the amended map of the dedicated soil-ecological units of the cadastral office, provide data on the update of the bonized soil-ecological units in the exchange format of the cadastral information system, including the application for registration in the cadastral.
(1) The Catastral Authority will implement the result of the update to the real estate cadastral of the protected soil units.
(2) The Land Authority shall, on the date of validity of the amended maps of Bonified Soil Organic Units, update to the national database of Bonified Soil Organic Units, thereby terminating the update of Bonified Soil Organic Units.
(3) The Land Authority shall inform the administrative authorities referred to in Article 5 (3) in writing of the termination of the update of the Bonized Soil Organic Units, including the date of validity of the amended Map of the Soil Organic Units.
Repeal
They shall be deleted:
1. Decree of the Ministry of Agriculture No. 327 / 1998 Coll., laying down the characteristics of the soil and the procedure for their management and updating.
2. Decree No. 546 / 2002 Coll., amending Decree No. 327 / 1998 Coll., laying down the characteristics of the soil and the procedure for their management and updating.
Efficacy
This Decision shall enter into force on 1 January 2019.
Minister:
Ing. Toman, CSc., v. r.
Příloha č. 1
Annex No 1 to Decree No 227 / 2018 Coll.
Climate regions
| Číselný kód regionů | Symbol regionů | Charakteristika regionů | Suma teplot nad 10 °C | Průměrná roční teplota v °C | Průměrný roční úhrn srážek v mm | Pravděpodobnost suchých vegetačních období v % | Vláhová jistota ve vegetačním období |
|---|---|---|---|---|---|---|---|
| 0 | VT | velmi teplý, suchý | 2800 - 3100 | 9 - 10 | 500 - 600 | 30 - 50 | 0 - 3 |
| 1 | T1 | teplý, suchý | 2600 - 2800 | 8 - 9 | < 500 | 40 - 60 | 0 - 2 |
| 2 | T2 | teplý, mírně suchý | 2600 - 2800 | 8 - 9 | 500 - 600 | 20 - 30 | 2 - 4 |
| 3 | T3 | teplý, mírně vlhký | 2500 - 2800 | (7) 8 - 9 | 550 - 650 (700) | 10 - 20 | 4 - 7 |
| 4 | MT1 | mírně teplý, suchý | 2400 - 2600 | 7 - 8,5 | 450 - 550 | 30 - 40 | 0 - 4 |
| 5 | MT2 | mírně teplý, mírně vlhký | 2200 - 2500 | 7 - 8 | 550 - 650 (700) | 15 - 30 | 4 - 10 |
| 6 | MT3 | mírně teplý (až teplý), značně vlhký | 2500 - 2700 | 7,5 - 8,5 | 700 - 900 | 0 - 10 | > 10 |
| 7 | MT4 | mírně teplý, vlhký | 2200 - 2400 | 6 - 7 | 650 - 750 | 5 - 15 | > 10 |
| 8 | MCH | mírně chladný, vlhký | 2000 - 2200 | 5 - 6 | 700 - 800 | 0 - 15 | > 10 |
| 9 | CH | chladný, vlhký | pod 2000 | < 5 | > 800 | 0 | > 10 |
Příloha č. 2
Annex No 2 to Decree No 227 / 2018 Coll.
Main soil units
01 Black countries modal, black countries carbonate, spray or Carpathian fleece, soils medium-heavy, mainly skeleton-free, to moderately skeletal in terraced gravel territory, very deep, beneficial to dry depending on the climate.
02 Black countries luvický, black countries luvický weakly glued on the spray cover, medium heavy, mainly without skeleton, to moderate skeletons in the terraced area, favourable to dry depending on the climate.
03 Black countries black, black countries black carbonates on deep scrubbers with clay, clinkers or terraces, medium-heavy, non-skeletous, or only with admixture, the rare possibility of a slight occurrence of skeletons, with a water regime favourable to slightly damp.
04 Black countries arenic on sands or shallow sprays (maximum overlap of up to 0,3 m) stored on sands and gravel-sands, gravely mainly light to medium heavy lighter, non-skeletal to low-skeletal, strongly permeable soil with dry-out regime.
05 Black countries modal and black countries modal carbonate, black countries luvic and fluvish modal and carbonate on sprays with a power of 0,3 - 0,7 m on very permeable ground, medium to lighter medium-heavy, predominantly skeletal, isolated to weak skeletal, moderately dry, dependent on collisions in the growing season.
06 Black countries pelic, black countries pelic carbonates, black countries black pelic and black countries black pelic carbonates on very heavy substrates (clay, clinkers, carpathian fleas, tuphits, tufites and tertiary sediments), heavy to very heavy with lightened ornic horizon, rarely gravel, with a tendency of surface moisture in the profile.
07 Smokes of modal and pitch modal carbonate, black and black pelic countries black pelic and black countries vertical, always on very heavy substrates, all-profile heavy to very heavy, non-skeletal (to medium-skeletal), often surface-moistened periodically.
08 Black countries modal, brown countries modal and luvic, blue and, where appropriate, blue and luvic countries, including slightly glued varieties, washed away, where the transition horizon or substrate is cultured on a surface of more than 50%, on sprays, dust and landmarks, light medium and medium heavy, mostly with no skeleton to low-slope.
09 Mod grey countries, including poorly glued and greyish luvická on sprays, spray clay, medium-heavy, non-skeletous, rarely low-skinned, mainly with favourable hair conditions.
10 Brown-ground modal including weakly glued on the droppings, occasionally on the dust, medium heavy with slightly heavier bottom, without skeleton, with favourable hair conditions to dry.
11 Brown countries modal, including weakly glued to spray and soliflufying clay with the predominance of the spray material (dustovice), medium heavy with heavier subsoil, without skeleton, rarely slightly skeletal, mainly with favourable moisture ratios.
12 The brown countries of the modal, cambilands of the modal and of the luvic, all including slightly glued varieties on the slope (polygenetic) clay, medium heavy with heavy subsoil, to medium skeletal, waterborne, in the bottom with local moisture.
13 Brown countries of the modal, brown countries of the luvic, blue, blue and stratified, including weakly glued varieties on eolic substrates, and possibly slopes (polygenetic clay) with a power of between 0,3 and 0,6 m, placed on a very permeable substrate, non-skeletal to medium-skeletal, dependent on rain rainfall in the growing season.
14 Mod, brown, luvic, including weakly glued to dust or silkworm (s) or silkworm (s) with significant eolic admixture, moderate with severe subsoil, with favourable hair conditions.
15 Lubricating and brown luvic, locust bean (mould) including weakly glued varieties on sloping soil with eolic admixture, moderate and heavier subsoil, without skeleton to medium-skeletal, hair-friendly only with short-term moisture.
16 Mod and aubergines of arenics, possibly weak and glued on light to clay terraces, sandstone and gravel trees with overlay of sand dusters and dusters in power 0,3 to 0,6 m, gravely medium-heavy, to weak-skinned, less-favourable to negative.
17 Arenic and weakly glued Luvees, light, permeable substrates, without skeleton, rarely weakly skeletal, dry, collision or irrigation dependent.
18 Modal, cambic and travertine rendzins, moderate to severe, mild to moderate, less waterproof.
19 Pararerendzins of modal, cambic and leaching on the optics and hard sludges or calcareous landmarks, isolated and cambidized modal on the ground gravel, including weakly glued varieties, medium to heavy, weak to medium-skeletal, with a good hair regime up to short-term overmoistened.
20 Pelagic, dehusked and melanical, pelvic, pelvic and pararendzine soils, including weakly glued varieties, always on very heavy substrates, clays, clinkers, flysci, tertiary sediments, heavy spores of basic rock and the like, heavy to very heavy, soil with low water permeability, mostly without skeleton, but also moderately skeletal.
21 Soils of arenic subtype, regolands, pararendzins, cambilands, or even fluvides on light, non-water-resistant, highly dry substrates, not skeleton-free to highly skeletal.
22 Soils such as the previous main soil unit (HPJ) 21 on slightly heavier substrates of the aluminium sand type or sandy clay with a water regime slightly more favourable than the previous.
23 Regolands of arenic, even slightly glued and glide, arenic and slightly glued on clay sands and gravel or terraces, lying on impermeable ground of clays, clinches, fleas, light to lighter medium-heavy up to 0.4-0,5 m, with heavy to very heavy lowlands, non-skeletous terraces, isolated and strong skeletons, the water regime is very volatile, depending on the depth of the impermeable well and the power of the overlay.
24 Cambiases of modal eubasic to mesobasic as well as pelic cambilands, including weakly glued varieties, from migrated slopes of carbonate-silicate rocks - flyshes and culm shale, medium to severe, to medium-skeletal, with medium water resistance.
25 Modal and dehusked, eubasic to mesobasic, exceptionally pellic, including weakly glued varieties on leavings and hard slivers, calcareous sandstone, clay sediments of marine neogene, medium-heavy fleas, permocarbonic, medium-heavy to medium-skeletal, soil with good water capacity.
26 Cambiages of modal eubasic and mesobasic, including weakly glued varieties on shale, snakes, slender base rocks, or indistinguishable rotation of base rocks with neutral to acidic (e.g. clay band, some metamorphosed diabases, etc.) predominantly moderate to moderate, with favourable hair conditions.
27 Cambilands of modal eubazic to mesobasic, including weakly glued varieties on sandstone, crumbs, curling iron, brda cambria, flyshes, gravelly light or moderate light, to mid-skeletal, dry soil.
28 Modal eubasic Cambiases, Modal eutrophic Cambiages, including weakly glued varieties on basic and ultra-basic rocks and their tufts, predominantly moderate, without skeleton to moderate, with favourable humidity ratios, medium-deep profiles and sloping positions mostly drier.
29 Cambilands of modal eubasic to mesobasic, including weakly ogled varieties, on rulas, spores, phylites, amphibolites, gabras, gabrodiorites, undifferentiated rotation of base rock, neutral, acidic, possibly granite, medium to medium-heavy, non-skeleton to medium-skeletal, with prevailing good hair conditions.
30 Cambiases of modal eubasic to mesobasic, pararendzins of modal and cambizines, pararendzins and chromic cambizates, ploughed, including slightly glued varieties, on the slopes of sedimentary rocks, sandstone, permocarbonon, flyshes, mostly medium heavy lighter to medium heavy, to medium-skeletal, hair-friendly to dry.
31 Arentic, eubasic to mesobasic, pararendzins arenic, pararendzins cambic arenic, including weakly ogled varieties, on sedimentary, mineral-poor substrates - sandstone, chalk sprays, permocarbonic, always light, without skeleton to medium-skeletal, low-water, dry.
32 Cambilands of modal eubasic to mesobasic, arenic, including poorly ogled varieties, on rough spores, permeable, mineral-poor substrates, granite, syenites, granodiorites, gabrodiorites, quartz diorites, less orthorulas, light with higher grus content, no skeleton to medium-skeletal, permeable, more dry, more moisture-friendly.
33 Cambiases of modal eubasic to mesobasic and mould chromic, pelic cambiages, pelic pararendzines, including weakly glued varieties, on heavy permocarbon spores, both heavy and medium-heavy, without skeleton to medium-skeletal conditions, with favourable hair conditions.
34 Dystric, mould-mesobasic, cryptopod-modal, cambioblozole-arenic, including weakly glued varieties, on all soil-forming substrates of light gravel rock, light to medium-heavy lighter, non-skeleton to medium-skeletal, lukewarm to moist, but always in a slightly cold climate region.
35 Dystric, mesobasic, cryptopodzoles, including weakly glued varieties, on all reinforced soil-forming substrates, medium-heavy, without skeleton to medium-skeletal, hair-friendly to slightly moist, in a slightly cool climate region.
36 Modular cryptopods, soils, dystric and / or mesobasic cambiosis, including weakly glued varieties, with no distinction of matte rocks, mostly medium heavy lighter, without skeleton to medium-skeletal, soil up to slightly moisturised but always in a cool climate region.
37 Lithic cambilands, ranker cambilands, blue rankers, lithic pararendzins on solid substrates without distinction, in suborns from 0.3 m high-skeletal or solid rock, light to lighter medium-heavy (9 KR i moderate and heavy), up to 0.3 m low to moderate-skeletal, exceptionally strong skeletal, mostly dry, dependent on precipitation.
38 Soils such as the previous HPJ 37, granular but moderate to severe, due to granular composition with better water resistance.
39 Litocountries modal and almost all lithic subtypes of other soil types on substrates without distinction, with shallow rough horizon usually 0.1 to 0.15 m high, with the origin of solid rock, with different granularity, with unfavourable moisture ratios.
40 Soils with a gradient of more than 12 degrees, on all substrates, gravelly medium to light, with various skeletons, moisture-dependent climate and exposure.
41 Soils with a slope of more than 12 degrees, gravelly medium to very heavy, with various skeletons, with somewhat more favourable lukewarm conditions.
90 Brown countries glued to dust (dust), solids with the predominance of spray material, sprays, medium heavy, mainly without skeleton, less to slightly skeletal, with a tendency to temporarily moisturise.
43 Brown countries of luvic glued, glued to dust (dustings), solids with the predominance of the spray material, medium heavy, in the bottom or heavier, mainly without a skeleton or with only a mixture of less to slightly skeletal, with a tendency to moisture.
44 Pseudogles of the modal, pseudogles of the luvický, on the dusty soil, solids with the predominance of the spray material, medium heavy, heavier in the bottom, without skeleton or with admixture, less to slightly skeletal, with a tendency towards temporary contamination.
45 Brown countries glued to slope (polygenetic) clay, often with an eolic admixture, moderate, without skeleton to weak skeletal, rarely moderate, with a tendency to temporary contamination.
46 Brown areas of luvic, glued, glued to the slopes (polygenetic) of clay, medium heavy, heavy in the bottom, without skeleton to medium skeletal, with a tendency to temporarily infested.
47 Pseudogles, pseudoglés of luvické, cambilands of glued and glide on sloping (polygenetic) clay, medium heavy, in the bottom heavier, without skeleton to medium skeletal, with a tendency towards temporary infestation.
48 Gloves, pararendzins, gagged, pararendzes, gagged and pseudogles on the leaves, shale, crumbs, permocarbonone or flyshes, isolated basic spills and tuphes, moderate to moderate, non-skeletal, with a tendency to temporary, mostly spring infestation.
49 Pelican-ogled, pararendzins of pelice-ogled, pararendzins of cambic pelice-ogled and pellodden-oglued on clay spores of slate, oils and hard hens, permocarbonone, flyshes, tufts and bazaic glues, gravely to very heavy, to moderate, with a higher tendency to temporary contamination.
50 Cambiages oglised and glide, pseudo-glouses modal, cambic, dystric on granite, rulls, spores, phylites, ryolites, dacites, ryolite tufts, porphyres, porphyrites, keratophyres, jingles, trachy, amphiboliths, gabras, gabrodiorites, snakes, perodites, picrites and opaques, basic outbreaks and their tuphes with lighter moderate earth and on all substrates in KR 9, predominantly moderate to moderate, mild to moderate, with a tendency to temporary contamination.
51 Gluvial, pseudo-goggle, glide, ground-gravel, terraces and morons, granular light or medium-heavy, non-skeleton to medium-skeletal, irregular water-dependent regime.
52 Pseudogles of modal and cambic, cambilands glued on light sediments of the limic tercier (freshwater upper-wing and tertiary deposits), often with the addition of an eolic material, (gravel-sand with a heavier base, especially in the area of eastern Bohemia), usually only slightly skeletal, moderately heavy to light, with a tendency to temporary moisture.
Pseudogles of pelican, planic, modal, cambic, cambilands geared to the heavier sediments of the limic tercier (freshwater supra-chalk and tertiary deposits), medium to medium heavy with heavier subsoil, only rarely medium-skeletal, low water-permeable, periodically infested.
54 Pseudogles of pelice and plaice, ogled pellet, oglised pellet, pelican-ogled cambilands, pelican-ogled pararendzins, pelican-ogled regolands, saliva-ogled clays, marine neogen and flyše clay sediments, with very adverse physical properties.
55 Psefitic, arenic, stratified (exceptionally weakly glued and slightly glide) and arenic (black), including carbonate subtypes on light nil deposits, often underlaid with terraces, glaciofluvial gravel, without skeleton to weak skeletons, generally sandy, dry.
56 Fluids of modal eubasic to mesobasic, cambic, stratified fluvides, including carbonate subtypes and glued and glide varieties on internal deposits (> 0,7 m), often with background terraces, glaciofluvial cleavage, moderate to moderate, generally with no skeleton to slightly skeletal, hair-friendly.
57 Pelic and cambic effluents eubasic to mesobasic, stratified fluvides, including carbonate subtypes and glued and glide varieties on heavy nil deposits, heavy to very heavy, generally with no skeleton to low skeletal, humid ratios favourable to moisture.
58 Glucose and glacial fluvores (> 0,7 m), with or without a terrace, medium or medium-heavy lighter (exceptionally light), without skeleton to low skeletal level, water level below 1 m, hair conditions unfavourable.
59 Glucose and glacial fluvores on nil deposits, heavy and very heavy, with no skeletons up to weak skeletons, hair conditions unfavourable.
60 Worm and Worm of modal carbonate, Arenic Worm, Fluvic Worm on the Native Sauces, Spray, Spray and Solufluc, medium heavy, lighter medium heavy, without skeleton to low skeletal, favourable hair conditions up to slightly moistened.
61 Pelican and black pelican carbonates on nil deposits, spray and soliflufying clay, dusts, clays and clinkers, flyshes, limnican terciers, heavy and very heavy, without skeletons up to slightly skeletous, prone to moisture.
62 Glej, glej carbonate, glej, dross, spray and saltwater clay, medium and light medium heavy, with no skeleton to low skeletal, temporarily contaminated with lower water fluctuating at a depth of 0,5 m - 1 m
63 Black pelice and carbonate on the nil deposits, dust and solivative clay, clays and clinkers, flyshes, limnican tertiary, heavy and very heavy, without skeleton to slightly skeletal, unfavourable hair ratios due to high water levels.
64 Modal gloss, modular stagnolia, fluvical gloss, cambic gloss, glide pseudogloss on the slope clay, nil deposits, clay and clinker materials, savoury, with modified water regime, medium to very heavy, without skeleton or slightly skeletal, hair ratios in the drainage function relatively favourable.
65 Aquatic, histic, modal matured, glide organosoil, histic stagnogles, matured stagnogles, (surface glues) on nil deposits, slopes, limic tertiary rocks and flyzes, light to very heavy with a higher content of organic substances, humidifying than HPJ 64, high-quality meadow under functional drainage.
Stagnogles of modal, histic, pelican, planic on sand, clay, clinkers and nil deposits, light to very heavy with higher content of organic substances, without skeletons to weak skeletons, very unfavourable water regime, difficult to perform meliorations.
67 Glej, pseudoglej on various substrates often steeply stored, in positions of wide depression and planar units, lighter moderate to moderate to very heavy, without skeleton to slightly skeletal, water-dependent on the level of flow, difficult to drain.
68 Glees, including matured, gleasy, gleek, matured on sand, clay, clinkers, slopes, (nil deposits) around smaller watercourses, soil of narrow depression including slopes, difficult to define, mainly without skeletons to moderate skeletons, lighter medium to very heavy water regime.
69 Aquatic glasses, aquarium matured glues, histic glasses (organosoil) on dtto HPJ 68 substrates, mainly heavy, heavily contaminated, soil depression and planar units.
70 Glasses of modal, fluvice and glidic fluvize on the nil deposits, or with a base of terraces, broad nives - width above 50 m on left and right side of the flow, lighter medium to very heavy, without skeletons to weak skeletons, with increased water levels in the flow suffering from flooding.
71 Fluvc, glidic fluvid, (maggot fluvice, glidic fluvure significantly moisturizes) the same properties as HPJ 70, narrow nives - below 50 m from the flow, often suffer from flooding.
72 Glasses of fluvice matured and glasses of fluvice histic, (organosoil) on nil deposits, possibly with a base terrace, lighter medium heavy, medium to very heavy, without skeleton or slightly skeletal, permanently under the influence of water level in the flow.
73 Glej and hypo-eluvized, hypo-eluvized, surface-eluvized, cambic, cathodes of soils located in slope positions, generally contaminated with the presence of slope springs, light medium to very heavy, to medium-skeletal.
74 Glej and hydroeluvized pseudogles, surface matured glasses and surface histic glasses, aquarium glues, hydroeluvized glues, modal stagnogles, soil lighter medium to very heavy, to medium-skeletal, cathode soils located in slope positions, infested, with sloping springs to spring with stagnating water, often matured.
75 Glej, pseudoglés and globes, cathodes of lower slopes, difficult to define transitions, on deluvias of rocks and slopes, lighter medium to very heavy, to moderate skeletal conditions, different humidity conditions.
76 Pseudoglés, globes of modal, matured and histic, organolands, cathnas with the predominance of hydromorphic soils, always with significant peat and contamination, with difficult availability, usually medium to very heavy, to moderate skeletal.
77 Shallow slits up to a depth of 3 m with the occurrence of colluvitions, regolands, camblands and others, with erosion lotions of orns, various granularities, non-skeletal to severe skeletons, with different hair conditions, not suitable for agricultural use.
78 Deep drains exceeding 3 m, with an uncharted representation of hydromorphic soils - glees, pseudogles and colluviuses of all subtypes with different, rather unfavourable humidity conditions, unsuitable for agriculture.
79 Arenic, arenic, colluvian, carbonated, colluvian, resulting from the imposition of light-bearing earths of > 0,5 m, light, non-skeletal, or with a mixture of coarse sand (grus), rarely low skeletal, hair ratios of little favourable, a tendency to elasticity.
80 Modal, modal carbonate colouvidaries, modal low-glued colouvidas resulting from the storage of light medium and medium-rare deborated earths > 0,5 m, light medium to medium-heavy, without skeleton to low-skeletal, favourable water regime.
81 Pelic, pelican-carbonate, colluvian, glued by the storage of heavy-bearing earths > 0,5 m, heavy to very heavy, without skeleton to low-skeletal, degraded water, possibility of periodic overhydration.
82 Humous andropos, allied andropos, including weakly glued varieties, as well as carbonates, with an overlay of 0,3 m above various materials, lighter moderate to moderate, with an addition of skeleton to medium-skeletal, hair conditions quite favourable.
83 Humous anthropolies, social anthropolies, pelic anthropolies, including weakly glued varieties, as well as carbonates, anthropodes glued with a cover of humous soil of up to 0,3 m (up to 0,4 m including transitional horizon) over various materials, heavy to very heavy, with an admixture of skeleton to medium-skeletal, possibility of local moisturization.
84 Humous anthropolies, anthropolies covered, and carbonates with an overlay of humous soil up to 0,3 m (up to 0,4 m including the transitional horizon) over light material, medium heavy (lighter medium heavy), below light, with an addition of skeleton to medium-skeletal, isolated and strongly skeletal, more dry by the power of the overlay.
85 Deep humic androposoil, even carbonates with overlay of humous soil above 0,3 m above various material, lighter medium to medium heavy, without skeleton to slightly skeletal, hair conditions favourable.
86 Deep humid and carbonate anthropolies with an overlay of humous soil above 0,3 m above various material, heavy to very heavy, without skeleton to slightly skeletal, periodically overhydrated.
87 Society andropos, agglomic andropos, glide andropos, humid andcarbonate, weakly glued varieties - cathodes of soil with soil inequality, hair ratios on the surface variable, soiling and water stagnation, various granularities, without skeleton to medium-skeletal.
88 Humous and / or deep-humic andropos, urbic and anti-humid earth, skeletal, overlay, reduced, sulphid, contaminated, intoxicated, intoxicated, even carbonates, possibility of gluing, overlapping with humic and non-humid soil by the deponification of urban waste, landfill sites, strongly skeletal materials from construction activity, contaminated to intoxicated material from the desalination sites, urban sludge, waste after mining of ores, direct anthropogenic material wipes the characteristics and sequence of horizons of the original HPJ, granality different (mostly moderate), free of skeleton to severe skeletous, hair ratios variable.
89 Glej anthropojí, with grainy from light to heavy, which can be variable both on the surface and in the profile, without skeleton to strongly skeletal, soil profile significantly hydromorphically affected (4-5 degree), hair conditions very unfavourable.
Příloha č. 3
Annex No 3 to Decree No 227 / 2018 Coll.
Impairment and exposure
Slope
| Kategorie | Rozpětí ve stupních | Charakteristika |
|---|---|---|
| 0 | 0 - 1 | úplná rovina |
| 1 | 1 - 3 | rovina |
| 2 | 3 - 7 | mírný sklon |
| 3 | 7 - 12 | střední sklon |
| 4 | 12 - 17 | výrazný sklon |
| 5 | 17 - 25 | příkrý sklon |
| 6 | nad 25 | sráz |
Exposure
It expresses the location of BPEJ's territory vis-à-vis world parties in four categories marked by codes 0 - 3.
| Kategorie | Charakteristika |
|---|---|
| 0 | se všesměrnou expozicí |
| 1 | jih (jihozápad až jihovýchod) |
| 2 | východ a západ (jihovýchod až severovýchod, jihozápad až severozápad) |
| 3 | sever (severozápad až severovýchod) |
In the climate regions (referred to in Annex No 1) for code numbers 0, 1, 2, 3, 4 and 5, exposure south is considered negative, other exposure is considered equal.
In the climatic regions (according to Annex No 1) for code numbers 6, 7, 8 and 9, exposure to the north is considered negative and other exposure is considered equal.
In the fourth place of the five-digit BPEJ code, the combination of inclination and exposure is coded as follows:
| Číselný kód | Kategorie sklonitosti | Kategorie expozice | |
|---|---|---|---|
| Klimatický region | |||
| 0 - 5 | 6 - 9 | ||
| 0 | 0 - 1 | 0 - 3 | 0 - 3 |
| 1 | 2 | 0 - 3 | 0 - 3 |
| 2 | 2 | 1 | 1 - 2 |
| 3 | 2 | 2 - 3 | 3 |
| 4 | 3 | 1 | 1 - 2 |
| 5 | 3 | 2 - 3 | 3 |
| 6 | 4 | 1 | 1 - 2 |
| 7 | 4 | 2 - 3 | 3 |
| 8 | 5 - 6 | 1 | 1 - 2 |
| 9 | 5 - 6 | 2 - 3 | 3 |
Příloha č. 4
Annex No. 4 to Decree No. 227 / 2018 Coll.
Skeletonicity and soil depth
Skeletonicity
| Kategorie | Charakteristika | Obsah skeletu |
|---|---|---|
| 0 | bezskeletovitá, s příměsí | do 10% |
| 1 | slabě skeletovitá | 10 - 25% |
| 2 | středně skeletovitá | 25 - 50% |
| 3 | silně skeletovitá | nad 50% |
The skeleton content is expressed by the total density of gravel (solid rock from 4 to 30 mm) and stone (solid rock from 30 mm).
Soil depth
It expresses the depth of part of the soil profile limited either by solid rock or by strong skeletons.
| Kategorie | Hloubka půdy | Charakteristika kategorie |
|---|---|---|
| 0 | > 60 cm | půda hluboká |
| 1 | 30 - 60 cm | půda středně hluboká |
| 2 | < 30 cm | půda mělká |
In the fifth place of the five-digit code, the code of the combination of skeletal and soil depth is given primarily as follows:
| Číselný kód | Skeletovitost | Hloubka | ||
|---|---|---|---|---|
| Kategorie | Charakteristika | Kategorie | Charakteristika | |
| 0 | 0 | bezskeletovitá, s příměsí | 0 | hluboká |
| 1 | 0 - 1 | bezskeletovitá až slabě skeletovitá | 0 - 1 | hluboká, středně hluboká |
| 2 | 1 | slabě skeletovitá | 0 | hluboká |
| 3 | 2 | středně skeletovitá | 0 | hluboká |
| 4 | 2 | středně skeletovitá | 0 - 1 | hluboká, středně hluboká |
| 5 | 1 | slabě skeletovitá | 2 | mělká |
| 6 | 2 | středně skeletovitá | 2 | mělká |
| 7+) | 0 - 1 | bezskeletovitá až slabě skeletovitá | 0 - 1 | hluboká, středně hluboká |
| 8+) | 2 - 3 | středně až silně skeletovitá | 0 - 2 | hluboká, středně hluboká, mělká |
| 9+) | 0 - 3 | bezskeletovitá až silně skeletovitá | 0 - 2 | hluboká, středně hluboká, mělká |
+) Applies only to soil of > 12 degrees, i.e. HPJ 40, 41.
1) Paragraph 8 (4) of Act No. 139 / 2002 Coll., on Land Adjustments and Land Offices, as amended.
2) Paragraph 1 (6) of Act No. 503 / 2012 Coll., on the State Land Office and on the amendment of certain related laws, as amended. § 8 (5) of Act No. 139 / 2002 Coll., as amended.
3) For example, § 15 of Act No. 334 / 1992 Coll., on the Protection of the Agricultural Soil Fund, as amended by Act No. 10 / 1993 Coll., § 15 (5) of Decree No. 13 / 1994 Coll., which provides for certain details of the protection of the Agricultural Soil Fund.
4) § 62 paragraph 1 of Act No. 256 / 2013 Coll., on the cadastral property of the Czech Republic (cadastral law).
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Regulation Information
| Citation | Decree No. 227 / 2018 Coll., on the characterisation and management and updating of the soil units |
|---|---|
| Regulation Type | - |
| Author | - |
| Collection | Code of Laws |
| Date of Promulgation | 12.10.2018 |
|---|---|
| Effective from | 01.01.2019 |
| Effective until | - |
| Status | Valid |
The regulation text is for informational purposes only.
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