ANSI ASTM F2651-2010 Standard Terminology Relating to Soil and Turfgrass Characteristics of Natural Playing Surfaces《用天然比赛表面土壤和人工草皮特征相关的术语》.pdf
《ANSI ASTM F2651-2010 Standard Terminology Relating to Soil and Turfgrass Characteristics of Natural Playing Surfaces《用天然比赛表面土壤和人工草皮特征相关的术语》.pdf》由会员分享,可在线阅读,更多相关《ANSI ASTM F2651-2010 Standard Terminology Relating to Soil and Turfgrass Characteristics of Natural Playing Surfaces《用天然比赛表面土壤和人工草皮特征相关的术语》.pdf(4页珍藏版)》请在麦多课文档分享上搜索。
1、Designation: F2651 10 (Reapproved 2015) An American National StandardStandard Terminology Relating toSoil and Turfgrass Characteristics of Natural PlayingSurfaces1This standard is issued under the fixed designation F2651; the number immediately following the designation indicates the year oforiginal
2、 adoption or, in the case of revision, the year of last revision. A number in parentheses indicates the year of last reapproval. Asuperscript epsilon () indicates an editorial change since the last revision or reapproval.1. Scope1.1 This terminology defines characteristics of soils andturfgrass for
3、use in the development of standards and specifi-cations for natural playing surfaces. This standard includesterms that pertain to natural playing surfaces used for sportsand may include those surfaces supporting the growth ofturfgrass or unvegetated (bare soil) playing surfaces that areconstructed w
4、ith natural materials.1.2 The terms defined in this terminology standard areappropriate for use by sports field development professionals,owners and institutions, installers and contractors and otherpractitioners in matters concerning natural surfacesevaluations, test methods, specifications, mainte
5、nance andconstruction.2. Terminologyaeration, ncondition and sum of all processes affecting soilpore-space gaseous composition, particularly with respect tothe amount and availability of oxygen for use by soil biota orsoil chemical oxidation reactions, or both.aeration, vpractice to mechanically res
6、tore a soil to acondition where gas and water permeability rates are im-proved and bulk density is lowered (decompaction) by theuse of devices (spikes, cores, tines, air-jets, water-jets) whichpenetrate into the soil profile. See also aerification, soil andcultivation, turf.aerification, soil, nmech
7、anical process to relieve soil com-paction. This term is often used synonymously with aeration,v (that is, mechanical aeration). See also aeration, v.bulk density, nmass of dry soil per unit bulk volume. Thevalue is expressed as Mg per cubic metre (Mg m3) or gramper cubic centimetre (g cm3).clay, nc
8、an be defined in terms of a particular size fraction ofa soil, a soil textural class, a soil particle size class, a soiltextural group, soil mineralogy, or, in engineering terms, asmaterials that exhibit plastic soil properties when at appro-priate water contents.DISCUSSIONIdeally, the term “clay” s
9、hould be appropriately definedwhen used to describe soils or materials for rootzones. For example, a90 % sand/10 % clay mixture could imply either 90 % sand/10 %clayey soil (or other soils with textures containing enough clay (2.0 mm and 0.05 mm and 85 % sand), ntypes of soils which may haveno (or a
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