This page contains a Flash digital edition of a book.
Sand is a cornerstone ingredient in all construction and maintenance materials for both natural and artificial playing surfaces.


Whether mixed with an organic amendment to produce topdressings, rootzones and divot mixes, or used on its own as a synthetic carpet infill or beach sport surface, sand plays a vitally important role in a playing surface’s performance, appearance and longevity.


Ruffords Technical Manager, Mick Higgins, explains what sand is and introduces some basic considerations


right one for your project. S


What is sand and where does it come from?


Sand is an inorganic granular mineral composed of individual particles or grains formed by the weathering and erosion of rock.


These small, finely divided fragments


of rock will vary in chemical composition depending upon the source and condition of the parent rock from which they were derived.


As far as the UK is concerned, sand


refers to a material which has a grain size distribution between 0.063mm and 2.0mm. However, there are some countries, including the USA, who categorise sand particles as those having a diameter between 0.053mm and 2.0mm.


In the UK all particles less than 0.063mm but greater than 0.002mm are classed as silt, with particles less than 0.002mm categorised as clay. Any particles greater than 2.0mm are categorised as gravel. It is important to remember that any particle between 0.063mm and 2.0mm would be classed as sand, including material with very high


and comes in many different forms, all of varying quality with a range of properties and physical characteristics, so the challenge is to select the


calcium content (calcareous sands). The majority of sands quarried in the UK consist mainly of silicon dioxide (SiO2


),


otherwise known as silica. There are, in fact, nine different crystalline forms of silica, but most of us associate it with quartz silica. In this form it has a high melting point and is also inert, stable and extremely hard wearing. Surface hardness of sand grains can be measured using the Mohs scale of mineral hardness, which measures the ability of a harder mineral to scratch a softer mineral. This scale ranges from 1, being the softest (talc), up to 10 being the hardest (diamonds). Typically, sands containing high silica content would have a hardness of around 7 using the Mohs scale.


The actual percentage of silica in sands can vary from around 80% up to 99.99%. Industrial silica sands are characterised by their high silica content (above 95% SiO2


), which is


usually in the form of quartz. Generally, whiter, paler coloured sands have fewer impurities. Typical impurities would normally include Iron oxide (Fe2 Alumina (Al2


O3 O3 ), however, surface clays,


feldspar, pyrite, chromite, coal, lignite, sea shells or chloride salts could be present.


The terms: silver sand, beach sand, soft sand, sharp


) and


Sand for


sportsturf


Page 1  |  Page 2  |  Page 3  |  Page 4  |  Page 5  |  Page 6  |  Page 7  |  Page 8  |  Page 9  |  Page 10  |  Page 11  |  Page 12  |  Page 13  |  Page 14  |  Page 15  |  Page 16  |  Page 17  |  Page 18  |  Page 19  |  Page 20  |  Page 21  |  Page 22  |  Page 23  |  Page 24  |  Page 25  |  Page 26  |  Page 27  |  Page 28  |  Page 29  |  Page 30  |  Page 31  |  Page 32  |  Page 33  |  Page 34  |  Page 35  |  Page 36  |  Page 37  |  Page 38  |  Page 39  |  Page 40  |  Page 41  |  Page 42  |  Page 43  |  Page 44  |  Page 45  |  Page 46  |  Page 47  |  Page 48  |  Page 49  |  Page 50  |  Page 51  |  Page 52  |  Page 53  |  Page 54  |  Page 55  |  Page 56  |  Page 57  |  Page 58  |  Page 59  |  Page 60  |  Page 61  |  Page 62  |  Page 63  |  Page 64  |  Page 65  |  Page 66  |  Page 67  |  Page 68  |  Page 69  |  Page 70  |  Page 71  |  Page 72  |  Page 73  |  Page 74  |  Page 75  |  Page 76  |  Page 77  |  Page 78  |  Page 79  |  Page 80  |  Page 81  |  Page 82  |  Page 83  |  Page 84  |  Page 85  |  Page 86  |  Page 87  |  Page 88  |  Page 89  |  Page 90  |  Page 91  |  Page 92  |  Page 93  |  Page 94  |  Page 95  |  Page 96  |  Page 97  |  Page 98  |  Page 99  |  Page 100  |  Page 101  |  Page 102  |  Page 103  |  Page 104  |  Page 105  |  Page 106  |  Page 107  |  Page 108  |  Page 109  |  Page 110  |  Page 111  |  Page 112  |  Page 113  |  Page 114  |  Page 115  |  Page 116  |  Page 117  |  Page 118  |  Page 119  |  Page 120  |  Page 121  |  Page 122  |  Page 123  |  Page 124  |  Page 125  |  Page 126  |  Page 127  |  Page 128  |  Page 129  |  Page 130  |  Page 131  |  Page 132  |  Page 133  |  Page 134  |  Page 135  |  Page 136  |  Page 137  |  Page 138  |  Page 139  |  Page 140  |  Page 141  |  Page 142  |  Page 143  |  Page 144  |  Page 145  |  Page 146  |  Page 147  |  Page 148