Effect of Soil Type and Fertilizer Application Timing on Phosphorus Leaching From Gypsum-Treated Agricultural Soils

dc.contributor.advisorJacinthe, Pierre-Andre
dc.contributor.authorCox, Kristiana
dc.contributor.otherWang, Lixin
dc.contributor.otherGilhooly, William P., III
dc.date.accessioned2021-01-04T08:51:36Z
dc.date.available2021-01-04T08:51:36Z
dc.date.issued2020-12
dc.degree.date2020en_US
dc.degree.disciplineDepartment of Earth Scienceen
dc.degree.grantorIndiana Universityen_US
dc.degree.levelM.S.en_US
dc.descriptionIndiana University-Purdue University Indianapolis (IUPUI)en_US
dc.description.abstractPhosphorus is an essential plant nutrient and an important contributor to the eutrophication of aquatic ecosystems. Studies have shown that gypsum (CaSO4∙H2O) applications can potentially reduce phosphorus export from agricultural fields. Most studies have examined the effect of gypsum application rates on treatment effectiveness, but limited research has been conducted to determine how the timing of gypsum application can affect soil phosphorus mobility and phosphorus leaching. A greenhouse experiment was conducted to address this question and further our understanding of the effect of gypsum addition on soil phosphorus chemistry. For the experiment, two soil types with different background phosphorus levels (low P, high P), and three different time intervals between gypsum and phosphorus fertilizer application (2, 28 and 56 days) were applied. A total of 18 soil columns (L: 15 cm; diam: 10 cm) packed with sieved soil were treated with gypsum (3.9 g) and separated into three sets corresponding to each of the phosphorus application times. An equal number of columns not treated with gypsum were also included to serve as controls. Phosphorus fertilizer (0.34 mg P cm-1) was added as KH2PO4 solution. Rainwater (58 mL) was applied every 2-4 days to generate leachate that was collected and analyzed for ortho-P, total P, and SO4-2. At the end of each time series, the set of soil columns were sliced into 2-4 cm increments, and water extractable and bicarbonate extractable phosphorus (Olsen-P) was determined to examine downward phosphorus movement. Results of the study showed that Olsen-P levels were not affected by the gypsum treatment, indicating no interference of gypsum treatment with the P-supplying capacity of soils. The gypsum treatment reduced water-extractable P levels in the high-P soil, but treatment effect was not significant in the low-P soil. Likewise, in the high-P soil, gypsum treatment resulted in leachate ortho-P reduction during the second and third period of collection. For the low-P soil, there was no significant reduction in ortho-P. Overall, these results indicated that the beneficial effect of gypsum on phosphorus export from agricultural fields is dependent on soil-P status and time interval between gypsum amendment and P fertilizer application.en_US
dc.identifier.urihttps://hdl.handle.net/1805/24748
dc.identifier.urihttp://dx.doi.org/10.7912/C2/564
dc.language.isoen_USen_US
dc.subjectPhosphorusen_US
dc.subjectGypsumen_US
dc.subjectSoilen_US
dc.subjectLeachingen_US
dc.titleEffect of Soil Type and Fertilizer Application Timing on Phosphorus Leaching From Gypsum-Treated Agricultural Soilsen_US
dc.typeThesisen
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