Decree of the Ministry of Agriculture No. 327 / 1998 Coll.
Decree of the Ministry of Agriculture laying down the characteristics of the soil and the procedure for their management and updating
Valid
Order
Effective from 31.12.1998
Text versions:
01.01.2003
31.12.1998
327
DECLARATION
Ministry of Agriculture
of 15 December 1998
laying down the characteristics of the soil-protected ecological units and the procedure for their management and updating
The Ministry of Agriculture provides pursuant to § 8 (8) of Act No. 284 / 1991 Coll., on Land Adjustments and Land Offices, as amended by Act No. 38 / 1993 Coll. and Act No. 217 / 1997 Coll.:
Characterisation of soil-protected ecological units
The BPEJ 1 is characterised by the climate region, the main soil unit, the inclination and exposure, the skeletons and the depth of the soil, which specify the main soil and climatic conditions of the land under assessment,
(a) the climate region comprises areas with approximately identical climatic conditions for the growth and development of agricultural crops, as set out in Annex No 1; it is expressed as the first digit of the five-digit code (1) (hereinafter referred to as the code number);
(b) the main soil unit is a dedicated grouping of soil forms of related characteristics that are determined by the genetic soil type, subtype, soil-forming substrate, granularity, soil depth, hydromorphism level, where appropriate by significant gradient or morphology of the terrain and by the fertilisation measure, as specified in Annex 2; it is expressed by the second and third digit of the code number;
(c) the inclination and exposure to the parties to the world shall reflect the shape of the surface of the agricultural parcel, as specified in Annex 3; it shall be expressed by the fourth digit of the code number resulting from their combination;
(d) skeleticity, which is the proportion of the gravel and stone content in the orchard to the gravel and stone content in the base of not more than 60 cm, and the depth of the soil, as referred to in Annex 4; it is expressed by the fifth digit of the code number resulting from their combination.
BPEI Management
(1) BPEJ is uniformly guided (2) in numerical and mapping terms in the national BPEJ database (hereinafter referred to as the "national database"), which contains information on soil quality. The management of the national database is provided by the Ministry of Agriculture (3) through an expert organisation which also provides on request summary information on BPEJ and its special-purpose groupings, e.g. for area and quality protection of land and water, for spatial planning, assessment of environmental stability of the landscape, development of economic instruments in agriculture and regional development.
(2) The documentation of the national database includes:
(a) maps of BPEI in digital and graphic form;
(b) information expressing climatic and soil conditions related to BPEI;
(c) records of the update of the BPEI;
(d) details of BPEJ's presence in the cadastral territory;
(e) the BPEJ special-purpose groups in the cadastral territory.
BPEI Update
(1) The update of BPEJ (hereinafter referred to as "update") is a finding of changes in the soil and climatic conditions of agricultural parcels by means of field surveys and their evaluation against the conditions that characterise the BPEI so far, for example where there have been obvious and substantial changes due to flooding, landslides, significant degradation and destruction of soil erosion, a fundamental change in the hydromorphism of the soil or, in the absence of a manifest earlier determination of BPEJ, etc. The updates shall be verified and specified, thereby defining, the new boundaries of different BPEI or, where appropriate, the code number BPEJ. An update shall also be considered as a finding of BPEJ data on land where BPEJ has not previously been identified. The reason for the update is also the need to supplement and specify the national database. 4) Updates under this decree are not affected by changes to the BPEJ's course of borders by the inaccuracy of the drawings and correction of errors arising from map printing. The update resulting in the modified BPEJ maps is provided by the Land Authority (5) through an expert organisation which enters the implementation in accordance with a specific regulation. 6)
(2) The map documents for the digital update and, where appropriate, the graphic form are:
(a) the maps referred to in Article 2 (2) (a) on the scale of the cadastral map;
(b) cadastral maps;
(c) copies of maps of earlier land records on the scale of the cadastral map showing parcels registered in the cadastral register in a simplified manner. 7)
(3) The Land Office, having found reasons for updating it within the meaning of paragraph 1, taking into account the requirements submitted by the owners of agricultural parcels, shall notify the opening and the scope of the update, including the date of the field survey and its conditions, and the place where proposals for changes to the BPEJ maps and after the update of the already amended BPEJ map will be made public.
(4) The Land Office shall request the municipality in whose territorial area the parcels concerned by the update of the BPEI are located to publish the notification referred to in paragraph 3 in a normal manner and the opening of the update of the BPEI and its scope shall separately inform the cadastral authority, the agricultural holding fund authority, (8) the tax office and the department of the Ministry of Agriculture.
(1) The Land Office shall ensure that the draft changes to BPEJ maps are unloaded (displayed on the translucent as an attachment to the map material referred to in Article 3 (2) or as a combination thereof) for a period of 30 days for public consultation. To that end, the Land Authority shall request the municipality to inform the public, in a manner customary, of the place where the draft changes to the BPEJ maps will be laid down and of the time limit by which such a proposal may be consulted and of the time within which each person may make written submissions to the Land Office. The comments made later will not be taken into account.
(2) Following evaluation of the public's observations received, the Land Office shall, on the basis of the results of the update, amend the BPEJ maps on the map referred to in Article 3 (2) (b) or (c), or both of the maps referred to in Article 3 (2) (b) and (c), indicating the date of their validity on the amended BPEJ maps and thereby terminating the update of the BPEJ. The Land Authority shall inform the authorities referred to in Paragraph 3 (4) in writing of the termination of the BPEJ update and shall also request the municipality to publish a notice on the termination of the BPEJ update in the usual manner.
Efficacy
This decree shall take effect on the day of its publication.
Minister:
Ing. Fencl v. r.
Příloha č. 1
Annex No. 1 to Decree No. 327 / 1998 Coll.
Characteristics of climate regions
| Číselný kód regionů | Symbol regionů | Charakteristika regionů | Suma teplot nad 10°C | Průměrná roční teplota°C | Průměrný roční úhrn srážek v mm | Pravděpodobnost suchých vegetačních období v procentech | Vláhová jistota |
|---|---|---|---|---|---|---|---|
| 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 | MT 1 | mírně teplý, suchý | 2400 - 2600 | 7 - 8,5 | 450 - 550 | 30 - 40 | 0 - 4 |
| 5 | MT 2 | mírně teplý, mírně vlhký | 2200 - 2500 | 7 - 8 | 550 - 650 (700) | 15 - 30 | 4 - 10 |
| 6 | MT 3 | mírně teplý (až teplý), vlhký | 2500 - 2700 | 7,5 - 8,5 | 700 - 900 | 0 - 10 | > 10 |
| 7 | MT 4 | mírně teplý, vlhký | 2200 - 2400 | 6 - 7 | 650 - 750 | 5 - 15 | > 10 |
| 8 | MCH | mírně chladný, vlhký | 2000 - 2200 | 5 - 6 | 700 - 800 | 0 - 5 | > 10 |
| 9 | CH | chladný, vlhký | pod 2000 | < 5 | > 800 | 0 | > 10 |
Příloha č. 2
Annex No 2 to Decree No. 327 / 1998 Coll.
Characteristics of main soil units
01 Black countries modal, black countries carbonate, spray or Carpathian fleece, medium-heavy soil, skeleton-free, very deep, mostly with favourable water regime
02 Luvic black countries on spray cover, medium heavy, without skeleton, mainly with favourable water regime
03 Black countries black, black countries black carbonates on deep scrubbers with clay, clinkers or terraces, medium heavy, non-skeletal, with water-friendly to slightly damp
04 Black countries of arenics on sand or shallow dusts (maximum overlap of up to 30 cm) stored on sand and gravel, grainy light, non-skeletal, strongly permeable soil with dry conditions
05 Black countries modal and black countries modal carbonate, black countries luvic and fluvish modal and carbonate on sprays with a power of 30 to 70 cm on very permeable ground, medium heavy, predominantly skeletal, medium dry, dependent on collisions in the growing season
06 Black countries pelic and black countries black pelic on very heavy substrates (clay, mink, Carpathian fleece and tertiary sediments), heavy to very heavy with an attenuated ornic horizon, rarely gravel, with a tendency of surface moisture in the profile
07 Foods of modal and pitch modal carbonate, black earth pelic and black land black pelic, always on very heavy substrates, all-profile very heavy, non-skeletal, often surface-moistened periodically
08 Black and black countries of pelic, brown, luviac and, where appropriate, luvic, washed, where a transition horizon or substrate is cultured on a surface of more than 50%, on dust, dust and silkworms, medium or heavy, mainly without skeletons and in a higher inclination
09 Mod grey land including slightly glued and grey luvic land on sprays, medium heavy, non-skeletal, with favourable hair conditions
10 Brown-ground modal including weakly glued on the wash, medium heavy with slightly heavier bottom, without skeleton, with favourable hair conditions up to dry
11 Brown-ground modal including weakly glued on spray and soliflufying clay (dustings), medium heavy with heavier base, without skeleton, with favourable humidity conditions
12 Mod, modal and luvic brown countries, all including weakly glued forms on slope (polygenetic) dirt, medium heavy with heavy bottom, 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, on eolic substrates and, where appropriate, slopes (polygenetic clay) with a maximum power of 50 cm on a very permeable substrate, non-skeletal to moderate skeletal, dependent on rainfall in the growing season
14 Mod, brown, luvic, including weakly glued on spray clay (dustings) or sloping (polygenetic) clay with significant eolic admixture, medium heavy with heavy subsoil, with favourable hair ratios
15 Mod and brown lube, including glued varieties on steep clay with eolic admixture, moderate to severe, to moderate-skeletal, hair-friendly only with short-term moisturization
16 Luvezí modal and brownish arenic, possibly and weakly glued on light to clay terraces, sandstone and gravel with overlay of sand dusters and dusters in the power of 30 to 60 cm, gravely medium heavy, up to slightly sceletous, slightly less favourable to negative
17 Arenic and weakly glued Luvees, light, permeable substrates, dry, collision or irrigation dependent
18 Modal, cambic and travertine rendzins, moderate to severe, mild to moderate, less waterproof
19 Pararerendzins, modular, cambic and leaching on leachs and hard clinkers or calcareous slopes, medium to severe, weakly to moderately skeletal, with a good hair regime up to short-term overmoistened
20 Pelvic and pararendzine soils on very heavy substrates, clays, clinkers, tertiary sediments and the like, soils with low water permeability, mainly without skeletons, but also with moderate skeletons, often slightly glued
21 Soils of an arenic subtype, regolands, pararendzins, Cambilands, or even fluvides on light, non-water-resistant, highly dry substrates
22 Soils such as the previous HPJ 21 on slightly heavier substrates of the aluminium sand type or sand clay with a water regime slightly more favourable than the previous
23 Regolands of arenic and cambilands of arenic nature, in both cases slightly gagged on clay sands and gravel or terraces, lying on impermeable ground of clays, clinkers, flyzes and tertiary clays, the water regime is highly volatile, depending on the depth of the impermeable layer and the power of the overlay
24 Cambivores of modal eubasic to mesobasic and pelic territories from displaced slopes of carbonatosilicate rocks - flyshes and culm shale, medium to severe, to moderate, with medium water resistance
25 Modular and extruded cambilands, eubasic to mesobasic, exceptional and pelic cambilands on plaques and hard clinkers, medium heavy flyscis, permocarbonone, medium to medium-sized, medium-sized, soil with good water capacity
26 Modal eubasic and mesobasic cambilands on shale, mainly moderate to moderate, with favourable hair conditions
27 Cambilands modal eubasic to mesobasic on sandstone, crumbs, curling iron, brda cambria, fleas, granular light or medium heavy light, with various skeletons, dry soil
28 Cambilands of modal eubasic, cambilands of modal eutrophic on basic and ultrabasic rocks and their tufts, predominantly moderate to moderate, without skeleton, with favourable humidity ratios, moderately deep
29 Cambilands of modal eubasic to mesobasic including weakly glued varieties, on rulas, spores, phylites, or granite, medium to medium-heavy lighter, without skeleton to medium-skeletal, with prevailing good hair conditions
30 Eubasic to mesobasic Cambilands on slopes of sedimentary rock - sandstone, permocarbon, fly, medium heavy lighter, to medium-skeletal, hair-friendly to dry
31 Cambilands modal to arenic, eubasic to mesobasic on sedimentary, mineral-poor substrates - sandstone, chalk opposites, permocarbon, but always light, without skeleton to medium-skeletal, low-water, dry
32 Cambilands modal eubasic to mesobasic on rough spores, permeable, mineral-poor substrates, granite, syenites, granodiorites, fewer orthorulas, medium-heavy with higher grus content, hair-friendly in humidifying climate
33 Cambiland modal eubasic to mesobasic and cambiland modal rubified on heavier permocarbon spores, heavy and moderate, sometimes moderate, with favourable hair conditions
34 Dystric, mould and cryptopodzola cambiobiles modal on granite, rulas, spores and phylites, medium to medium-scale, light to medium-scale, lukewarm, but always in a slightly cool climate region
35 Dystric, Mesobasic, cryptopod-modal cambilands including weakly glued varieties, shale, permocarbonate, flyshes, neutral gilt rocks and their slopes, medium to moderate, medium-skeletal, hair-friendly to slightly moist, in a slightly cool climate region
36 Modular cryptopodzoles, modal podzoles, dystric cambizas, possibly mesobasic cambizem, with no distinction of matte rocks, mostly medium heavy lighter, with various skeletons, soils to slightly moistened but always in a cold climate region
37 Lithic, modular, ranker, and mould-based, non-differentiated solid substrates, suborbital from 30 cm deep-rock or solid rock, light to light in the eagle, 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 Lithium Modal on substrates without distinction, with shallow rough horizon with solid rock origin, usually 10 to 15 cm powerful, with unfavourable moisture ratios
40 Soils with a gradient of more than 12 degrees, cambilands, rendzins, pararendzins, rankers, regolands, black countries, browns and others, granular medium to light, with various skeletons, water-dependent and exposure
41 Soils as with HPJ 40 but gravelly medium to very heavy with somewhat more favourable hair conditions
42 Brown countries glued to dust (dust), dust, medium heavy, non-skeleton, with a tendency to temporarily moisturize
43 Luvic brown countries, glued to dust (dusters), medium heavy, in the bottom or heavier, without skeleton or with only admixture, with a tendency to moisturise
44 Modal pseudoglés, Luvic pseudoglés, on dusty clay, medium heavy, heavy in the bottom, without skeleton or with admixture, with a tendency to be temporarily infested
45 Brown countries glued to steep (polygenetic) clay, often with an eolic admixture, medium heavy, without skeleton to slightly skeletal, with a tendency towards temporary contamination
46 Brown countries of luvic, glued, glued to slope (polygenetic) clay, medium heavy, heavy in the bottom, non-skeletal to moderate, with a tendency towards temporary contamination
47 Pseudogles modal, pseudoglés luvické, cambilands glued on slope (polygenetic) clay, medium heavy, heavier to moderate in the bottom, with a tendency towards temporary infestation
48 Cambiages of oglised, rendzine of cambic oglised, pararendzins of cambic oglised and pseudogles of modal on the opacity, shale, permocarbonate or flyshes, moderate to moderate, without skeleton to moderate, with a tendency towards temporary, mostly spring infestations
49 Pelican, glued, pelvic, paraphrase, cambic, pelvic, glandular and pellowish, glued on clay spores of slate, permocarbonon and flyses, tuphes and basic spills, grainy to very severe to moderate skeletal, with a higher tendency to temporary contamination
50 Cambilands of ogled and pseudogles, modular on granite, runes and other solid rocks (which are not in HPJ 48,49), moderate to moderate, slightly to moderately skeletal, with a tendency towards temporary contamination
51 Globe-glued and pseudoglate-modal cambicountry with clay gravel, terraces and moray, grained light or medium-heavy light, without skeleton to medium-skeletal, with irregular water-dependent rainfall
52 Pseudogles of modal, cambilands glued on light sediments of the limic tercier (freshwater upper-wing and tertiary deposits), often with the addition of an eolic material, usually only slightly skeletal, grained medium to light, with a tendency to temporarily moisturise
Pseudogles of pelican flat, cambilands glued to the heavier sediments of the lim tercier (freshwater upper-wing and tertiary deposits), medium to severe, only occasionally medium-skeletal, low water-permeable, periodically infested
54 Pseudoglia pelican, ogled pellet, ogled pellet pellet, pelican-ogled cambicountry, pelican-oglish pararendzine, saliva, marine neogen and flysh clays, and limic tertiary clay sediments, heavy to very heavy, with very unfavourable physical properties
55 Psefitic, arenic stratified, arenic and pararendzines on light nil deposits, often underlaid with terraces, generally sandy, dry
Fluid modal eubasic to mesobasic, cambic, colluvian modal on a nil storage site, often underlaid with terraces, medium to moderate, generally without skeleton, hair-friendly
57 Flexibility of pelic and cambic eubasic to mesobasic on heavy nil deposits, up to very heavy, without skeleton, favourable humidity to moisture
58 Glucose fluvores on the nil deposits, possibly with a ground terrace, medium or medium heavy lighter, only slightly skeletal, water level below 1 m, water conditions favourable after drainage
59 Glasses on nil deposits, heavy and very heavy, without skeleton, moisture conditions unfavourable, require water control
60 Blue and black blue carbonate and arenic black on nil deposits, powder and dust clay, medium heavy, without skeleton, favourable hair conditions up to slightly moistened
61 Pelican and black pelican carbonates on nil deposits, dust, dust, clay and clinker, heavy and very heavy, without skeleton, prone to moisture
62 Glej, glej carbonate, glej, dross and dust, medium and light, without skeleton, temporarily contaminated with lower water fluctuating at a depth of 0,5 - 1 m
63 Pelican and carbonate pellets on nil deposits, clays and clinkers, heavy and very heavy, without skeleton, unfavourable hair ratios due to high water levels
64 Modular, stagnogal and fluvical glues on steep clay, nil deposits, clay and mucous materials, tufted, with modified water mode, medium to very heavy, without skeleton or slightly skeletal
65 Glasses of aquarium, histic, modal matured, organoland of glej on the nil deposits, slopes, rocks of limic terrier and fly, light to very heavy with higher organic content, moisturizes than HPJ 64
66 Stagnogles modal and histic on sand, clay, clinkers and foreign deposits, light to very heavy with higher content of organic substances, very unfavourable water regime, unsuitable for its treatment
67 Modal gloss on various substrates often stringed, in positions of wide depression and flat units, moderate to severe, water-dependent on flow level, flooded, hard to drain
68 Glasses of modal and modal matured, glasses of histic, maggot matured on nil deposits around smaller watercourses, soil of narrow depression including slopes, difficult to define, medium to very heavy, adverse water regime
69 Aquatic, aquarium, matured and histic glasses on the internal deposits or slopes, mainly heavy, heavily contaminated, soil depression and planar units
70 Glasses of modal, fluvice and glidic fluvizas on nil deposits, possibly with a terrace, with terraces of wide nebula, medium to very heavy, with increased water level in the flow suffering from flooding
71 Fluvický, fluvidy, the same properties as HPJ 70, but significantly moisturizes at the terraces of narrow nives
72 Glasses of fluvical matured and fluvical histic on the nil deposits, moderate to very heavy, permanently under the influence of water level in the flow
73 Glej and hydroeluvian, hydroeluvian and surface cambilands, found in slope positions, generally infested with the presence of slope springs, moderate to very heavy, to moderate skeletal
74 Glej and hydroeluvian pseudogles, surface-matured and surface-histic globes, aquarium globes, modal stagnoglate, medium to very heavy soils, to medium-skeletal areas located in slope positions, infested with sloping springs, often matured
75 Gleese, pseudoglés and globes, lowland areas of slopes, pollution more pronounced than in HPJ 74, difficult to define transitions, on delutions of rocks and slopes, to moderate skeletal
76 Pseudoglés, glasses matured and histic, organolands, always with significant peat and contamination, with difficult availability, generally medium to very heavy, skeletal
77 Shallow rafts up to 3 m deep with the occurrence of colluvitions, regolands, camblands and others, with erosion loops, various granularities, non-skeletal to severe skeletal, for agricultural use not suitable
78 Deep drains exceeding 3 m, with an uncharted representation of hydromorphic soils - glees, pseudoglees and colluviuses of all subtypes with significantly unfavourable humidity conditions, unsuitable for agriculture.
Příloha č. 3
Annex No. 3 to Decree No. 327 / 1998 Coll.
Characteristics of inclination and exposure
Slope
| Kód | Kategorie | 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 | 25° | sráz |
Exposure
It expresses the location of BPEJ's territory vis-à-vis world parties in four categories marked by codes 0 - 3.
| Kód | Charakteristika |
|---|---|
| 0 | se všesměrnou expozicí |
| 1 | jih (jihozápad až jihovýchod) |
| 2 | východ a západ (jihozápad až severozápad, jihovýchod až severovýchod) |
| 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 (as set out in Annex No 1) for code numbers 6, 7, 8 and 9, exposure to the north is considered as negative and exposure to the east - west and south is considered as equal.
In the fourth place of the BPEJ code number, the combination of inclination and exposure is coded as follows:
| Číselný kód | Kód sklonitosti | Kód expozice |
|---|---|---|
| 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 |
Příloha č. 4
Annex No. 4 to Decree No. 327 / 1998 Coll.
Characterisation of skeletal and soil depth
Skeletonicity
| Kód | Charakteristika | ||
|---|---|---|---|
| 0 | bezskeletovitá, s příměsí | s celkovým obsahem skeletu | do 10% |
| 1 | slabě skeletovitá | s celkovým obsahem skeletu | 10 - 25% |
| 2 | středně skeletovitá | s celkovým obsahem skeletu | 25 - 50% |
| 3 | silně skeletovitá | s celkovým obsahem skeletu | 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.
| Kód | Charakteristika | |
|---|---|---|
| 0 | > 60 cm | půda hluboká |
| 1 | 30 - 60 cm | půda středně hluboká |
| 2 | < 30cm | půda mělká |
In the fifth place of the code number, the code of the combination of skeleton and soil depth is given as follows:
| Číselný kód | Kód skeletovitosti | Charakteristika kódu skeletovitosti | Kód hloubky půdy | Charakteristika hloubky půdy |
|---|---|---|---|---|
| 0 | 0 | bezskeletovitá, s příměsí | 0 | hluboká |
| 1 | 0 - 1 | bezskeletovitá, s příměsí, | 0 - 1 | hluboká, středně hluboká |
| slabě skeletovitá | ||||
| 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, s příměsí, | 0 - 1 | hluboká, středně hluboká |
| slabě skeletovitá | ||||
| 8+) | 2 - 3 | středně skeletovitá, | 0 - 2 | hluboká, středně hluboká, mělká |
| silně skeletovitá | ||||
| 9+) | 0 - 3 | bezskeletovitá, s příměsí, | 0 - 2 | hluboká, středně hluboká, mělká |
| slabě skeletovitá, | ||||
| středně skeletovitá, | ||||
| silně skeletovitá |
+) Applies only to land with a gradient > 12 0, i.e. HPJ 40, 41 and HPJ 39 undeveloped (ranker) soils.
1) Paragraph 8 (8) of Act No. 284 / 1991 Coll., on Land Adjustments and Land Offices, as amended by Act No. 38 / 1993 Coll. and Act No. 217 / 1997 Coll.
2) Sections 13 (d) and 11 (b) of Act No 284 / 1991 Coll.
3) Article 31 of Act No. 576 / 1990 Coll., on the Rules of Management of the Budget Funds of the Czech Republic and the Municipality of the Czech Republic (Budget Rules of the Republic), as amended.
4) For example, Article 15 of Act No. 334 / 1992 Coll., on the Protection of the Agricultural Soil Fund, as amended by Act No. 10 / 1993 Coll., and Article 15 (5) of Decree No. 13 / 1994 Coll., which provides for certain details of the protection of the Agricultural Soil Fund.
5) Paragraph 11 of the Land Adjustment Act and Land Authorities Act.
6) Act No. 513 / 1991 Coll., Commercial Code, as amended.
7) Paragraph 28 (3) of Act No. 344 / 1992 Coll., on the cadastral property of the Czech Republic (cadastral law), as amended by Act No. 89 / 1996 Coll.
8) Act No. 334 / 1992 Coll., as amended.
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Regulation Information
| Citation | 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 |
|---|---|
| Regulation Type | Order |
| Author | - |
| Collection | Code of Laws |
| Date of Promulgation | 31.12.1998 |
|---|---|
| Effective from | 31.12.1998 |
| Effective until | - |
| Status | Valid |
The regulation text is for informational purposes only.
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