ADAS rooo TARM NG LANO & LE SURC. West Dorset Local Plan Objector Sites. Agricultural Land Classification

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\ o West Dorset Local Plan Objector Sites Agricultural Land Classification Prepared for MAFF by H C Lloyd Jones ADAS Statutory Unit Bnstol ADAS rooo TARM NG LANO & LE SURC ct? Ministry of Agriculturc Fisheries and Food MAFF Land Us«Fanning Unit M ^

WEST DORSET LOCAL PLAN OBJECTOR SITES AGRICULTURAL LAND CLASSIFICATION CONTENTS SUMMARY 1 INTRODUCTION 2 CLIMATE 3 COCKROAD FARM BEAMINSTER 4 LONGBURTON 5 THORNFORD Page 1 2 2 3 4 5 APPENDIX 1 References 7 APPENDIX 2 APPENDIX 3 Descnption of the grades and subgrades Definition of Soil Wetness Classes 8 10 \ MAPS

WEST DORSET LOCAL PLAN OBJECTOR SITES AGRICULTURAL LAND CLASSIFICATION SURVEY SUMMARY The survey was camed out by ADAS on behalf of MAFF as part of rts siatutory role in the preparation of the West Dorset Local plan The fieldwork covered sites at Beaminster Longburton and Thomford and was completed in September 1995 at a scale of 1 10 000 Data on climate soils geology and from previous Agncurtural Land Classification (ALC) Surveys was used and is presented in the report The distnbution of grades is shown on the accompanying ALC map and summansed t}elow Information is correct at this scale but could be misleading if enlarged Distnbution of ALC grades Cockroad Farm, Beammster % of % of Grade Area (ha) Survey Agncultural Area Land (6 2 ha) 4 6 2 912 Urban 0 2 3 0 0 0 Agncuttural Buildings 0 4 5 8 0 0 TOTAL 6 8 None of the agncuttural land in the survey at Cockroad Farm is best and most versatile The site has heavy clay loam topsoiis over gleyed slowly permeable clays which cause a severe wetness limitation All ofthe agncultural land was therefore mapped as Grade 4 Distnbution of ALC grades Longburton % of % of Grade Area (ha) Survey Agncultural Area Land (13 9 ha) 3a 2 8 19 3 20 1 3b 11 1 76 6 79 9 Non Agncuttural 0 6 4 1 0 0 TOTAL 14 5 20% Ofthe agncuttural land surveyed at Longburton is best and most versatile This Subgrade 3a mapping unrt consisted of shallow well drained clay loams over weathered lenticular limestone which suffer from a moderate drought limitation and in places a moderate depth limrtation The rest of the srte was mapped as Subgrade 3b due to a moderate wetness limitation The profiles in this mapping unrt have heavy clay loam topsoils over gleyed clay subsoils The clay honzons are slowly permeable layers Distnbution of ALC grades Thomford Grade Area (ha) %of Survey Area %of Agncultural Land (2 2 ha) 4 TOTAL 22 22 None of the site is best and most versatile The srte has heavy clay loam topsoiis over clay subsoils The subsoils are gleyed and slowly permeable causing a severe wetness limitation

INTRODUCTION An Agncuttural Land Classification (ALC) Survey was camed out in September 1995 at Beaminster Longburton and Thomford on behalf of MAFF as part ofrtsstatutory role in the preparation of the West Dorset Local Plan The fieldwork covenng 23 5 ha of land was conducted by ADAS at a scale of 1 10 000 wrth approximately one bonng per two hectares of agncuttural land A total of 27 auger bonngs were examined and four soil profile prts used to assess subsoil condrtions The recent surveys sufiersede any previous surveys having been camed out at a more detailed level and using the Revised Guidelines and Cntena for grading the quality of agncultural land (MAFF 1988) The survey at Beaminster expands upon the area covered by two previous surveys The Revised Guidelines and Cntena provide a framework for classifying land according to the extent to which rts physical or chemical charactenstics impose long term limitations on agncuttural use The grading takes account of the top 120 cm of the soil profile A descnphon of the grades used in the ALC system can be found in Appendix 2 CLIMATE The grade of the land is determined by the most limrting factor present The overall climate is considered first because rt can have an ovemding influence on restncting land to a lower grade despite other favourable conditions Estimates of climatic vanables were interpolated from the published agncuttural climate dataset (Meteorological Office 1989) The parameters used for assessmg overall climate are accumulated temperature a measure of the relative wamith of a locality and average annual rainfall a measure of overall wetness The results shown in Table 1 indicate there is no overall limrtation due to climate Table 1 Climatic Interpolations Cockroad Farm Beaminster Gnd Reference Altitude (m) Accumulated Temperature (day ) Average Annual Rainfall (mm) Overall Climatic Grade Field Capacrty Days Moisture defiat (mm) Wheat Potatoes ST 472 018 83 1488 988 1 198 92 80 Longburton Gnd Reference Artrtude (m) Accumulated Temperature (day ) Average Annual Rainfall (mm) Overall Climatic Grade Field Capaaty Days Moisture deficrt (mm) Wheat Potatoes ST 651 127 85 1477 897 1 188 98 89 ST 649 132 95 1465 886 1 186 97 86

Thornford Gnd Reference ST 606 136 Attitude (m) 55 Accumulated Temperature (day ) 1512 Average Annual Rainfall (mm) 853 Overall Climatic Grade 1 Field Capaaty Days 180 Moisture defiat (mm) Wheat 101 Potatoes 93 Climatic data on Field Capacity Days (FCD) and Moisture Defiats for wheat and potatoes are also shown These data are used in assessing the soil wetness and droughtiness limitations referred to in later sections 3 COCKROAD FARM BEAMINSTER 31 An area of 6 8 ha at Cockroad Farm Beammster Dorset was surveyed in Septemt>er 1995 A total of eight auger bonngs were examined and one soil profile prt was used to assess subsoil conditions The published provisional one inch to the mile ALC map of the area (MAFF 1974a) shows the grade of the site at a reconnaissance scale to be Grade 3 3 2 RELIEF AND LANDCOVER The srte occupies two fields on the north west edge of Beaminster The area is relatively fiat wrth all gradients being less than 7 The attitude drops from 85 m above ordnance datum (AOD) in the north east of the site to 75 m in the southem part of the srte At the time of survey the whole area was under permanent pasture 3 3 GEOLOGY AND SOILS The geology ofthe site is shown on the published 1 50 000 scale solid geology map sheet 327 (Instrtute of Geological Sciences 1977) This shows that most of the site is underlain by Fuller's Earth Clay although there is a small area of Infenor Oolite Limestone mapped along the Southem edge of the srte The soils were mapped by the Soil Survey of England and Wales in 1983 at a reconnaissance scale of 1 250 000 This shows the site to consist of soils from the Wickham 2 Association They are descnbed as being slowly permeable seasonally waterlogged fine loamy over clayey fine silty over clayey and clayey soils There may also be a small area of slowly permeable calcareous soils on the steep slopes The soils found dunng the recent survey were all heavy clay loams over slowly permeable clays as descnbed by the Wickham 2 Assoaation

3 4 AGRICULTURAL LAND CLASSIFICATION The distnbution of ALC grades is shown m Table 2 and on the accompanying ALC map This information could be misleading if shovtm at a larger scale Table 2 Distnbution of ALC grades Cockroad Fann, Beaminster % of % of Grade Area (ha) Survey Agncultural Area Land (6 2 ha) 4 6 2 912 Urban 0 2 3 0 0 0 Agncuttural Buildings 0 4 5 8 0 0 TOTAL 6 8 Grade 4 The land in this mapping unit has a severe wetness limrtation the profiles typically have a heavy clay loam topsoii over a grey clay sut>soil The subsoils are gleyed and are slowly penmeable layers The depth to the clay vanes behween 20 cm and 30 cm over the site so the profiles were assessed as Wetness Class IV (see Appendix 3) In places there are patches of fiints at the top of the subsoil but these do not affect the overall grade and limitation Other land The farmstead and buildings are mapped as such while two bungalov^ are mapped as urban land 4 LONGBURTON 4 1 An area of 6 8ha at Longburton was surveyed in September 1995 A total of sixteen auger bonngs were examined and two soil profile pits were used to assess subsoil conditions the published provisional one inch to the mile ALC map ofthe area (MAFF 1974b) shows the grade of the site at a reconnaissance scale to be all Grade 3 4 2 RELIEF AND LANDCOVER The site occupies land around the village of Longburton Dorset The area is relatively flat wrth all gradients less than 7** and falls from 105 m AOD along the westem edge to 90 m AOD in the east At the time of survey all the fields were under pemianent pasture 4 3 GEOLOGY AND SOILS The geology of the srte is shown on the published 1 50 000 scale solid and dnft geology map sheet 312 (Institute of Geological Saences 1973) This shows that the geology has a north south trend wrth most of the site being underlain by Forest Marble clay and lenticular limestone Near the stream in the north east part of the srte the geology is Combrash (nodular limestone) The soils were mapped by the Soil Survey of England and Wales in 1983 at a reconnaissance scale of 1 250 000 This shows that the whole srte consists of soils from the Shertxime Assoaation They are descntied as being shallow well drained brashy calcareous clayey soils over limestone They are assoaated with slowly penmeable calcareous clayey soils

The soils found dunng the recent survey were very similar to those descnbed above The fields adjacent to Long Burton Farm in the east and west have shallow well drained soils over limestone The rest of the site has heavy clay loam topsoils over slowly permeable clayey subsoils 4 4 AGRICULTURAL LAND CLASSIFICATION The dislnbution of ALC grades is shown in Table 2 and on the accompanying ALC map This information could be misleading if shown at a larger scale Table 3 Distnbution of ALC grades Longburton Grade Area (ha) %of Survey Area %of Agncultural Land (13 Sha) 3a 3b Non agncurtural TOTAL 28 11 1 06 14 5 193 76 6 41 20 1 79 9 00 Subgrade 3a The land in this mapping unrt has a moderate drought limitation and in places a moderate depth limitation The profiles are typically shallow well drained medium clay loam topsoiis over heavy clay loam subsoils The weathered Forest Marble bedrock was found in subsoil honzons with stone contents ranging from 60% to 90% hard rock by volume The depth at which these honzons started at vaned from 20 cm to 50 cm across the unrt tt is these high stone contents that cause the drought limitation and where the honzon is closer to the surface the depth limrtation The profiles were assessed as Wetness Class I Subgrade 3b Most of the srte has been mapped as Subgrade 3b wrth a moderate wetness limitation The profiles in this mapping unrt typically have a shallow heavy clay loam topsoii over a gleyed slowly permeable clay subsoil and were assessed as Wetness Class III Some areas had gleying starting higher up the profile and were therefore assessed as Wetness Class Iv but these profiles also had medium clay loam topsoiis and were therefore still also mapped as Subgrade 3b Other land A small area of woodland is mapped as non agncuttural land 5 THORNFORD 51 An area of 2 2 ha at Thomford was surveyed in September 1995 A total of three auger tx)nngs were examined and one soil profile prt was used to assess subsoil condrtions the published provisional one inch to the mile ALC map of the area (MAFF 1974b) shows the grade of the srte at a reconnaissance scale to be all Grade 3 5 2 RELIEF AND LANDCOVER The srte occupies one field on the northem edge of the village of Thomford Dorset The area is relatively fiat at an attrtude of 55 m AOD At the time of the survey the site was under rough grassland

5 3 GEOLOGY AND SOILS The geology of the srte is shown on the published 1 50 000 scale solid geology map sheet 312 (Institute of Geological Saences 1973) This shows that the whole of the srte is undertain by Fuller's Earth (earth limestone) The soils were mapped by the Soil Survey of England and Wales in 1983 at a reconnaissance scale of 1 250 000 as belonging to the Sherbome Assoaation They are descnbed as being shallow well drained brashy calcareous clayey soils over limestone They are assoaated with slowly permeable calcareous clayey soils The soils found dunng the recent survey were similar to the calcareous clays descnbed m the Shertx}me Assoaation They had heavy clay loam topsoiis over grey slowly p)ermeable clay subsoils 5 4 AGRICULTURAL LAND CLASSIFICATION The distnbution of ALC grades is shown in Table 3 and on the accompanying ALC map This information could be misleading if shown at a larger scale Table 4 Distnbution of ALC grades Thornford Grade Area (ha) %of Survey Area %of Agricultural Land (2 2 ha) 4 TOTAL 22 22 Grade 4 The whole of the srte has been mapped as Grade 4 due to a severe wetness limrtation The profiles consist of heavy clay loam topsoiis over gleyed slowly permeable clay subsoils The depth to the clay vanes between 20 cm and 35 cm over the site so the profiles were assessed as Wetness Class IV Resource Planning Team Taunton Statutory Unrt September 1995

APPENDIX 1 REFERENCES INSTITUTE OF GEOLOGICAL SCIENCES (1973) Solid and Dnfl Edrtion Sheet 312 Yeovil 1 50 000 INSTITUTE OF GEOLOGICAL SCIENCES (1977) Solid Edrtion Sheet 327 Bndport 150 000 MAFF (1974a) Agncuttural Land Classification Map Sheet 177 Provisional 1 63 360 scale MAFF (1974b) Agncurtural Land Classification Map Sheet 178 Provisional 1 63 360 scale MAFF (1988) Agncultural Land Classification of England and Wales (Revised Guidelines and Cntena for gradmg the qualrty of agncuttural land) Alnwick METEOROLOGICAL OFFICE (1989) Climatological Data for Agncuttural Land Classification SOIL SURVEY OF ENGLAND AND WALES (1983) Sheet 5 Soils of South West England 1 250 000 scale

APPENDIX 2 DESCRIPTION OF GRADES AND SUBGRADES Grade 1 -excellent quality agncultural land Land with no or very minor limitations to agncuttural use A very wide range of agncuttural and horticuttural crops can be grown and commonly include top frurt soft fruit salad crops and winter harvested vegetables Yields are high and less vanable than on land of lower quality Grade 2 - very good quality agncultural land Land wrth minor limitations which affect crop yield cuttivations or harvesting A wide range of agncultural and horticuttural crops can usually be grown but on some land m the grade there may be reducedflexibilrtydue to difficulties with the production of the more demanding crops such as winter harvested vegetables and arable root crops The level of yield is generally high but may be lower or more vanable than Grade 1 Grade 3 - good to moderate quality agncultural land Land wrth moderate limitations which affect the choice of crops timing and type of cultivation harvesting or the level of yield Where more demandmg crops are grown yields are generally lower or more vanable than on land tn Grades 1 and 2 Subgrade 3a good quality agncultural land Land capable of consistently produang moderate to high yields of a narrow range of arable crops espeaady cereals or moderate ytelds of a wide range of crops including cereals grass oilseed rape potatoes sugar beet and the less demanding horticuttural crops Subgrade 3b moderate quality agricultural land Land capable of producing moderate yields of a narrow range of crops pnncipally cereals and grass or lower yields of a wider range of crops or high yields of grass which can be grazed or harvested over most of the year Grade 4 poor quality agricultural land Land with severe limitations which significantly restnct the range of crops and/or level of yields It is mamly surted to grass wrth occasional arable crops (e g cereals and forage crops) Ihe yields of which are vanable In most climates yields ofgrass may be moderate lo high but there may be difficulties m utilisation The grade also includes very droughty arable land

Grade 5 - very poor quality agncultural land Land with very severe limitations which restnct use to penmanent pasture orroughgrazing except for occasional pioneer forage crops Descriptions of other land categones used on ALC maps Urban Buirt up or hanj uses with relatively little potential for a retum to agnculture including housing industry commerce education transport religious buildings cemetenes Also hard surfaced sports faalrties permanent caravan srtes and vacant land all types of derelict land including mineral workings which are only likely to t>e reclaimed using derelict land grants Non-agncultural Soft uses where most ofthe land could be retumed relatively easily to agncutture includmg pnvate parte land public open spaces sports fields allotments and soft surfaced areas on airports/airfields Also active mineral workings and refuse tips where restoration condrtions to soft after uses may apply Agncultural buildings Includes the normal range of agncuttural buildings as well as other relatively permanent structures such as glasshouses Temporary structures (e g polythene tunnels erected for lambing) may be ignored Open water Includes lakes ponds and nvers as map scale permits Land not surveyed Agncuttural land which has not been surveyed Where the land use includes more than one ofthe above landcover types e g buildings in large grounds and where may be shown separately Otherwise the most extensive cover type will usually be shown Source MAFF (1988) Agncuttural Land Classification of England and Wales (Revised Guidelines and Cntena for Grading the Qualrty of Agncultural Land) Alnwick

APPENDIX 3 DEFINITION OF SOIL WETNESS CLASSES Wetness Class I The soil profile is not wet within 70 cm depth for more than 30 days in most years Wetness Class II The soil profile is wet within 70 cm depth for 31 90 days in most years or if there is no slowly penmeable layer within 80 cm depth rt is wet withm 70 cm for more than 90 days but not wet within 40 cm depth for more than 30 days in most years Wetness Class III The soil profile is wet wrthin 70 cm depth for 91 180 days in most years or if there is no slowly permeable layer wrthin 80 cm depth rt is wet wrthin 7Q cm for more than 180 days but only wet wrthin 40 cm depth for between 31 and 90 days in most years Wetness Class IV The soil profile is wet wrthin 70 cm depth for more than 180 days but not wrthin 40 cm depth for more than 210 days in most years or if there is no slowly permeable layer wrthin 80 cm depth rt is wet wrthin 40 cm depth for 91 210 days in most years Wetness Class V The soil profile is wet wrthin 40 cm depth for 211 335 days in most years Wetness Class VI The soil profile is wet within 40 cm depth for more than 335 days in most years Notes The number of days speafied is not necessanly a continuous p>enod In most years is defined as more than 10 oul of 20 years Source Hodgson J M (in preparation) Soil Survey Field Handbook (revised edrtion) 10

SITE NAME Cock Road Farm Beaminster JOB NO 63/95 Honzon No Lowest Av Depta (cm) Texture PROFILE NO Prt 1 (ASP7) DATE 21/9/95 Matnx (Ped Face) Colours SLOPE AND ASPECT 3 South GRID REFERENCE ST473 018 Stoniness Size Type and Field Melhod Mottling Abundance Contrast Size and Colour LAND USE Pennanent Grass DESCRIBED BY HLJ Mangan Cones Av Rainfall ATO FCDays 198 Climatic Grade 1 Exposure Grade Structure Ped Development Consistence Size and Shape 988 mm 1488 day C Structural Condition Pores (Fissures) PARENT MATERIAL Fuller s Earta Clay (Limestone) SOIL SAMPLE REFERENCES None Roots Abundance and Size Calcium Carbonate Conlent Honzon Boundary DisUnctaess and form 1 24 HCL 10YR33 1 ^HR TOTAL (VIS) FFVFO (7 5YR58) None Good CF+VF Clear Smoolh 2 50+ C 10YR62 1%HR TOTAL (VIS) MDMO (10YR68) None WCAB Firm Poor Poor FF+VF Profile Gl^ed From 24cm Available Water Wheat 125 mm Final ALC Grade 4 Depta to Slowly Permeable Honzon 24cm Potatoes 102 mm Moisture Deficit Wheat 92 mm Main Limiting Factor(s) Wetness Wetness Class IV Potatoes 80 mm Wetaess Grade 4 Moisture Balance Wheat 33 mm Potatoes 22 mm Remarks Augured to 100cm Droughtiness Grade I (Calculated to 120 cm) RPT37afs