Data

Grade of soil pedal structure (grade)

Also known as: substrate_pedality, Grade of soil pedal structure (grade)
Atlas of Living Australia
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ctx_ver=Z39.88-2004&rft_val_fmt=info%3Aofi%2Ffmt%3Akev%3Amtx%3Adc&rfr_id=info%3Asid%2FANDS&rft_id=https://spatial.ala.org.au/layers&rft.title=Grade of soil pedal structure (grade)&rft.identifier=ala.org.au/uid_841&rft.publisher=Atlas of Living Australia&rft.description=Grade of pedality (soil pedal structure) is estimated as single grain (1), massive (2), weak (3), moderate (4), or strong (5). Pedality influences water flow and transport within soils and may influence susceptibility to erosion (Onweremadu et al. 2007; Williams 1992). Derived from McKenzie et al. (2000). This classification does not necessarily reflect an ordered property of the soil. See HPEDALITY for a hydrological scoring of pedality. &rft.creator=Anonymous&rft.date=2014&rft.coverage=northlimit=-9.0 southlimit=-43.8 westlimit=112.9 eastLimit=153.64 projection=WGS84&rft_rights=Permission required to re-distribute derivative works. Please contact Dr. Kristen Williams - kristen.williams@csiro.au&rft_subject=ENVIRONMENTAL SCIENCE AND MANAGEMENT&rft_subject=ENVIRONMENTAL SCIENCES&rft_subject=Substrate&rft_subject=Physics&rft.type=dataset&rft.language=English Access the data
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Permission required to re-distribute derivative works. Please contact Dr. Kristen Williams - kristen.williams@csiro.au

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Grade of pedality (soil pedal structure) is estimated as single grain (1), massive (2), weak (3), moderate (4), or strong (5). Pedality influences water flow and transport within soils and may influence susceptibility to erosion (Onweremadu et al. 2007; Williams 1992). Derived from McKenzie et al. (2000). This classification does not necessarily reflect an ordered property of the soil. See HPEDALITY for a hydrological scoring of pedality.

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Environmental Science and Management | Environmental Sciences | Physics | Substrate |

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  • Local : ala.org.au/uid_841
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