Dynamics of biosolids-derived phosphorus in a Mollisol

dc.contributor.advisor Michael L. Thompson
dc.contributor.author Sui, Yaobing
dc.contributor.department Department of Agronomy
dc.date 2018-08-23T12:51:03.000
dc.date.accessioned 2020-06-30T07:22:22Z
dc.date.available 2020-06-30T07:22:22Z
dc.date.copyright Fri Jan 01 00:00:00 UTC 1999
dc.date.issued 1999
dc.description.abstract <p>Land application of biosolids (treated municipal sewage sludge) is becoming more popular because it is an agronomically, environmentally, and economically acceptable means for biosolids disposal. When the amount of biosolids is applied to agricultural land according to N-based on agronomic rate, however, the amount of P applied is generally more than plants need. The subsequent accumulation of P is of environmental concern, because it could lead to eutrophication of water bodies if P is carried off-site in runoff water and eroded soils. Thus, a completely randomized block experiment with three biosolids treatments (control, low, and high biosolids application rates) and four blocks was designed for studying the fate of biosolids-derived P applied to a Mollisols. The research was focused on the redistribution of biosolids-derived P, the effect of biosolids on P in mobile soil solution and in groundwater, the changes in forms of soil P after biosolids application, and the effect of biosolids amendment on the P sorption, desorption, and buffering capacities of the soil. The results showed that (1) biosolids application at both low and high rates significantly increased total P concentration at the 0--25 cm depth of soils, (2) biosolids application at both rates significantly increased the P concentration in mobile soil solution collected at the 50 cm depth below soil surface, but the amount of P in mobile soil solution only accounted for 2% or less of P added in biosolids to soil surface, (3) biosolids application did not influence the P concentration in groundwater, (4) biosolids application at both rates significantly affected both absolute and relative concentration of P fractions at the 0--5 cm depth but not at the 20--35 cm depth of soils; at the 5--20 cm depth of soils, only some fractions of P were influenced, (5) P sorption, desorption, and buffering capacities were significantly influenced by biosolids application; P-binding energies and equilibrium P concentration were also significantly affected by the biosolids application, (6) the transformation of biosolids-derived P applied to soil has been observed from HCl-extracted P into H2O-extracted P and NaHCO3-extracted inorganic P, and probably into NaOH-extracted inorganic P, too.</p>
dc.format.mimetype application/pdf
dc.identifier archive/lib.dr.iastate.edu/rtd/12616/
dc.identifier.articleid 13615
dc.identifier.contextkey 6807949
dc.identifier.doi https://doi.org/10.31274/rtd-180813-13882
dc.identifier.s3bucket isulib-bepress-aws-west
dc.identifier.submissionpath rtd/12616
dc.identifier.uri https://dr.lib.iastate.edu/handle/20.500.12876/66004
dc.language.iso en
dc.source.bitstream archive/lib.dr.iastate.edu/rtd/12616/r_9924770.pdf|||Fri Jan 14 19:26:07 UTC 2022
dc.subject.disciplines Agriculture
dc.subject.disciplines Environmental Sciences
dc.subject.disciplines Soil Science
dc.subject.keywords Agronomy
dc.subject.keywords Soil Science (Soil morphology and genesis)
dc.subject.keywords Soil morphology and genesis
dc.title Dynamics of biosolids-derived phosphorus in a Mollisol
dc.type dissertation
dc.type.genre dissertation
dspace.entity.type Publication
relation.isOrgUnitOfPublication fdd5c06c-bdbe-469c-a38e-51e664fece7a
thesis.degree.level dissertation
thesis.degree.name Doctor of Philosophy
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