


Soil texture will be determined in the field by the feel method. Texture classes in the United States are represented by the texture triangle presented below. Flowcharts to assist in determining texture can be found at: http://cmase.pbworks.com/f/Soil+Texture+By+Feel.pdf.
Additional information may be found at:
http://www.ext.colostate.edu/mg/gardennotes/214.html
https://www.nrcs.usda.gov/wps/portal/nrcs/detail/soils/edu/?cid=nrcs142p2_054311
http://www.fao.org/fishery/static/FAO_Training/FAO_Training/General/x6706e/x6706e06.htm
http://passel.unl.edu/pages/informationmodule.php?idinformationmodule=1130447039&topicorder=2

Soil structure is defined as the combination or arrangement of primary particles into secondary units called peds. Soil structure is important because it affects water infiltration and movement through the soil, heat transfer, and aeration. Additions of organic matter will improve soil structure.
Types of structure in soils include granular, blocky, prismatic, columnar, and platy. Soils without a specific type of structure are called structureless and may be single grain or massive.
Additional information may be found at:
http://www.agriinfo.in/default.aspx?page=topic&superid=4&topicid=267
http://www.deeproot.com/blog/blog-entries/what-is-soil-structure-and-why-is-it-important
https://www.sciencedirect.com/topics/agricultural-and-biological-sciences/soil-structure
https://www.nrcs.usda.gov/wps/portal/nrcs/detail/soils/edu/?cid=nrcs142p2_054278