Roadstone - which rock? Investigating the best rock type for the wearing course of roads



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Roadstone - which rock? Investigating the best rock type for the wearing course of roads Roads are made of various types of rock aggregate (crushed rock fragments). Quarries provide the aggregate used in the construction of our roads. The rock type has to be carefully chosen so that it has suitable properties for the job it has to do. Pupils are asked to work out which rocks are the most suitable for use as roadstone aggregate. Show pupils the diagram of the cross section through a road surface (below) and provide them with copies of Table 1 (page 3) and tell them that many rock types are suitable for the lower three layers providing they have sufficient strength and are packed in such a manner as to be permeable. However, the top layer on which the traffic runs, the wearing course, takes much higher pressures and all the wear and tear of the traffic and of the weather. It is this wearing course which forms the main focus of this activity. Cross section through a typical road surface wearing course base course 35mm 75mm Provides a skid- and wear-resistant surface for the traffic and protects the lower layers. Distributes the traffic loads on the road base. road base Main load-bearing layer. made of rocks with high crushing strength 200mm Thicknesses of these layers are typical values and depend on the amount of traffic the road has to take. The rock aggregate and the bitumen matrix that hold it together are called asphalt Ask the pupils to suggest properties that the wearing course must have. It must provide a durable, skid-resistant surface and must prevent water percolating down to the lower layers. A much higher quality of rock is needed for this layer than for the other layers; only a few rock types are suitable, especially for motorways and other roads carrying much traffic. Give the pupils copies of the Pupil Information Sheet (page 4), Table 3 (page 5) and, if possible, provide the samples listed. If required, also give them copies of Tables 2a: Composition of rocks and Table 2b: Hardness of minerals and volcanic glass (page 3). Without Tables 2a and 2b this is a good revision exercise. bitumen matrix with fillers rock fragments (aggregate) Detail of the mineral grains within the rock fragment magnification x c.15 40mm The pupils should now complete Table 3 and decide which rocks are suitable for the wearing course of a road and which are not. Cross section through the wearing layer of a road with a detail of a rock fragment Diagrams by P. and M. Williams and reproduced with permission from Teaching Earth Sciences, Vol 39 No.2 2014 1

The back up Title: Roadstone - which rock? Subtitle: Investigating the best rock type for the wearing course of roads Topic: This investigation can be carried out as a revision exercise of the major rock types in science, environmental science, geography or economics lessons. Age range of pupils: 12 years and upwards Time needed to complete activity: 30 minutes Pupil learning outcomes: Pupils can: measure grain size of a selection of rocks; use six criteria to determine the best choice of rock for the wearing course of a road; appreciate that limestone is extensively used for the base course and road base because it is readily available. It is also used for the wearing course in areas where a lower specification is acceptable, such as car parks and private driveways. Context: Basalt, dolerite (and some other igneous rocks), and greywacke fulfil all six criteria and so are the best rocks to use for the wearing course, but their outcrops are not evenly distributed so transport costs are high. Rocks that are very poor are shale and oolitic limestone. Flint is very strong but would not be a good rock to use. It is made of one mineral and breaks into sharp angular pieces to which bitumen does not readily adhere. Following up the activity: Pupils could investigate local aggregate quarries to find out how the rock is used. It might be possible to arrange a visit. Underlying principles: Rocks used for aggregate for the wearing course of the best quality roads must:- - have most minerals with hardness greater than 5 to resist abrasion - be made of two or more minerals with different hardnesses so that the surface does not become polished - be fine- or medium-grained - be well-cemented or made of interlocking crystals to resist pressures and stresses - have rough surfaces so that bitumen will adhere - not be porous. If water could get in then frost would cause it to shatter in winter. Economics often determines which rocks are used. If the transport costs are too high for the best quality rocks to be used, then inferior quality aggregate may be used instead, especially on minor roads. The best quality aggregate is used on motorways and on roads which bear a great deal of traffic. Although crystalline limestone is not the best rock for the wearing course, it is widely distributed across the country and is extensively used for the lower courses of roads of all types. In practice, one of the best rocks for the wearing course of major roads is a type of sandstone, known as greywacke, quarried at Ingleton in North Yorkshire and in mid- Wales, among other sites. Greywacke is composed of and feldspar grains, with some clay matrix, cemented by iron oxides to form a tough rock. Its different components mean that it is worn away at different rates, so that it always maintains its skid resistant surface. Fine and medium-grained igneous rocks are extensively quarried from Charnwood Forest in Leicestershire. The central location in the country, and nearness to the motorway network, mean that the Charnwood roadstone features widely in English roads, in areas where other suitable rocks do not occur. Thinking skill development: By completing Table 3, the pupils are recognizing patterns. Discussion involves metacognition and looking at rocks that are unsuitable may cause cognitive conflict. Applying the relevant criteria to the sample rocks (or sample list) and working out which rocks are most suitable requires bridging skills. Resource list: copies of Table 1, the Pupil Information Sheet and Table 3. Tables 2a and 2b are optional samples of the rocks listed in Table 3, if possible hand lenses or magnifying glasses if rock samples are available grain scale cards or rulers. Useful links: The design and construction of roads - http://community.dur.ac.uk/~des0www4/cal/roads/index.html An idiot s guide to road maintenance - http://www.highwaysmaintenance.com/design.htm A guide to aggregate testing - http://www.northstonematerials.com/filestore/documents/aggre gate-tests.pdf SoE unit Bulk Constructional Minerals, York e-library http://www.nationalstemcentre.org.uk/elibrary/resource/1147/b ulk-constructional-minerals Source: Adapted from an original article by Dr. Mike Tuke, republished by Peter and Maggie Williams in Blasts from the past 3: Roadstones, Teaching Earth Sciences, Vol 39, No.2 2014. The Earthlearningidea Team is grateful to Clive Nicholas and Julian Smallshaw for their helpful advice in updating this activity. Julian Smallshaw is Head of Educational Development, The Institute of Quarrying. 2

TABLE 1 - ROAD LAYERS Name and thickness of layer Wearing course 13-38mm Base course 38-76mm Road base 102-204mm Sub-base Variable Purpose and composition of layer Provides a skid- and wear-resistant surface for the traffic and protects the lower layers. Distributes the traffic loads on to the road base. Main load-bearing layer. Made of rocks with high crushing strength Builds surface up to approximately the correct level. Made of large fragments so that water cannot rise by capillary action TABLE 2A: COMPOSITION OF ROCKS Igneous rocks Main minerals Andesite feldspar, hornblende, augite Basalt Dolerite Gabbro Granite feldspar,, mica Rhyolite feldspar,, mica, volcanic glass Obsidian volcanic glass Pumice volcanic glass FROM QUARRY.. Metamorphic rocks Marble calcite Gneiss, feldspar, mica, hornblende Quartzite Schist mica Slate mica Sedimentary rocks Flint Limestone Sandstone Greywacke Shale calcite, feldspar, clay minerals clay minerals.. TO ROAD TABLE 2B: HARDNESS OF MINERALS AND VOLCANIC GLASS Augite 6 Calcite 3 Clay minerals 2 5 Feldspar 6 Hornblende 6 Mica 2 5 Quartz 7 Volcanic glass 6 Top photo: Bardon Hill Quarry, Leicestershire, Peter Williams Bottom photo: Road mending in Sheffield, Peter Kennett 3

Roadstones - which rock? Pupil information sheet Good roadstone for making the wearing course of roads must have the following properties: 1. The majority of the minerals in the rocks must have a hardness greater than 5 so that the rock is able to resist the abrasion caused by the tyres of the vehicles. 2. The grains must wear in such a way that the exposed surface of the rock fragments (aggregate) does not become polished, otherwise the traffic would skid. This means that the rock must be made of two or more minerals with different hardnesses. surface of the road surface of the road augite plagioclase feldspar Mineral grains all the same i.e. in ite Rock fragments made of only one mineral wear to a flat surface which does not prevent vehicle skidding Several mineral grains e.g. dolerite When rock fragments are made of several different mineral grains with different hardnesses, then the rock fragments wear to a stepped surface which is skidresistant 2cm Detail of crystal wear in a rock fragment Worn road surface with aggregate raised above bitumen matrix 1 coin for scale Diagram and photograph by P. and M. Williams and reproduced with permission from Teaching Earth Sciences, Vol 39 No.2 2014 3. The rock needs to be fine- to medium-grained so that fragments 0.5cm in diameter contain grains of several different minerals. 4. The individual grains need to be strongly held together so that the aggregate does not crumble under the pressures and stresses exerted by the vehicles. This means the rock must be either well-cemented or made of interlocking crystals. 5. The aggregates must have rough surfaces so that the bitumen can adhere to them. Bitumen does not adhere well to glassy surfaces e.g. flint and obsidian, but it does adhere to most other rocks. 6. The rock of which the aggregate is made must not be porous otherwise freezing and thawing during the winter might shatter the rock. Earthlearningidea team. The Earthlearningidea team seeks to produce a teaching idea regularly, at minimal cost, with minimal resources, for teacher educators and teachers of Earth science through school-level geography or science, with an online discussion around every idea in order to develop a global support network. Earthlearningidea has little funding and is produced largely by voluntary effort. Copyright is waived for original material contained in this activity if it is required for use within the laboratory or classroom. Copyright material contained herein from other publishers rests with them. Any organisation wishing to use this material should contact the Earthlearningidea team. Every effort has been made to locate and contact copyright holders of materials included in this activity in order to obtain their permission. Please contact us if, however, you believe your copyright is being infringed: we welcome any information that will help us to update our records.if you have any difficulty with the readability of these documents, please contact the Earthlearningidea team for further help. Contact the Earthlearningidea team at: info@earthlearningidea.com 4

Table 3: Geology of Roadstone Examine each sample and for each:- 1. Measure its grain size (if it is too small to measure, put < 0.5mm) 2. Look up its mineral composition and list the minerals in the table below 3. Look up the hardness of each mineral and write it beside the mineral on the table 4. Complete the table by putting a tick where the rock satisfies the criteria 1-6 and a cross where it does not Rock Granite Gabbro Dolerite Basalt (not vesicular or amygdaloidal) Quartz sandstone, poorly cemented Greywacke, well cemented Shale Oolitic limestone Flint Quartzite Schist Slate Grain size Minerals with hardness of each 1 2 3 4 5 6 Which are the best three rocks for making the wearing course of a major road? 5 1. most minerals with hardness > 5 2. two or more minerals 3. grain size < 2mm 4. strong rock 5. bitumen adheres well 6. low porosity