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Exploring Mechanisms for the Development of Reversible Soil Hydrophobicity PDF

150 Pages·2013·1.77 MB·English
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AN ABSTRACT OF THE THESIS OF Priscilla B. Woolverton for the degree of Master of Science in Soil Science presented on June 7, 2013 Title: Exploring Mechanisms that Drive the Development of Reversible Soil Hydrophobicity Abstract approved: Maria I. Dragila Markus Kleber This study focuses on one widespread characteristic of poor soil quality: hydrophobic soil. Previous research has produced conclusive evidence to show that soil hydrophobicity is affected by soil organic matter (SOM) and soil water content (WC). Hydrophobicity that responds to changes in WC is a unique form of surface hydrophobicity and is termed “reversible hydrophobicity” (RHP). Recent experimental results support an amphiphilic model for SOM, which contains mechanisms for the occurrence of RHP. What has not been directly demonstrated, however, are conformational changes in the orientation of amphiphilic moieties as an effect of WC that would be associated with RHP. Quincy soils, which exhibit RHP, were investigated at varying WC using Photoacoustic Fourier transform infrared spectroscopy (Pas-FTIR), chemical analysis of carbon:nitrogen, and physical measurement of hydrophobicity, using the Capillary Rise Method and the Sessile Drop Method, in order to reveal how SOM and water interact to drive the creation of hydrophobic surfaces. This investigation suggests that SOM and water interact at the molecular scale to drive hydrophobic phenomena at the field-scale. ©Copyright Priscilla B. Woolverton June 7, 2013 All Rights Reserved Exploring Mechanisms that Drive the Development of Reversible Soil Hydrophobicity by Priscilla B. Woolverton A THESIS submitted to Oregon State University in partial fulfillment of the requirements for the degree of Master of Science Presented June 7, 2013 Commencement June, 2014 Master of Science thesis of Priscilla B. Woolverton presented on June 7, 2013. APPROVED: Co-Major Professor representing, Soil Science Co-Major Professor representing, Soil Science Head of the Department of Crop and Soil Science Dean of the Graduate School I understand that my thesis will become part of the permanent collection of Oregon State University libraries. My signature below authorizes release of my thesis to any reader upon request. Priscilla B. Woolverton, Author AKNOWLEDGEMENTS There are many people to whom I owe gratitude. First, I would like to express sincere admiration to my husband and family who have made the last few years possible. I would also like to especially thank Dr. Maria Dragila for her enduring patience and thoughtful insight. CONTRIBUTION OF AUTHORS Jess Holcomb assisted with soil sampling and chemical extraction data collection. Dr. Maria Dragila was involved with the design and writing of Chapters 1, 2 and 3, and assisted in the interpretation of the data. Dr. Markus Kleber was involved with the design and writing of Chapter 3 and assisted in the interpretation of the data. Dr. Don Horneck facilitated the oversight of all field-site activities, including soil sampling, field trial management and grower participation. TABLE OF CONTENTS Page 1. Introduction: Soil hydrophobicity................................................... 1 2. Characterization of soil wettability................................................. 11 2.1. Introduction.............................................................................. 11 2.2. Background............................................................................. 14 2.2.1 Quantifying soil wettability.............................................. 14 2.2.2 Theoretical support of physical soil wettability, and soil organic matter, measurements........................ 17 2.3. Materials and Methods........................................................... 23 2.3.1 Study site........................................................................ 23 2.3.2 Physical measurement of wettability and soil organic matter characterization...................................... 24 2.4. Results..................................................................................... 29 2.4.1 Comparison of Capillary Rise Method (CRM), moisture content, and carbon:nitrogen ratio................... 29 2.4.2 Sessile Drop Method (SDM) and Photoacoustic Fourier transform infrared spectroscopy (Pas-FTIR)..... 34 TABLE OF CONTENTS (Continued) Page 2.5. Discussion............................................................................... 41 2.5.1 Bulk-scale wettability: Comparison of results from CA(CRM) and C:N................................................. 41 2.5.2 Surface-scale wettability: Comparison of results from CA(SDM) and Pas-FTIR............................. 47 2.6. Conclusion............................................................................... 53 3. Photacoustic Fourier transform infrared spectroscopy to explore mechanisms of soil water repellency............................... 55 3.1. Introduction............................................................................. 55 3.2. Background: The nature of soil organic matter and its implications for soil hydrophobicity.......................................... 57 3.3. Materials and Methods............................................................ 64 3.3.1 Soil organic matter: Pas-FTIR and C:N......................... 64 3.3.2 Physical wettability........................................................ 68 3.4. Results..................................................................................... 69 3.5. Discussion............................................................................... 89 TABLE OF CONTENTS (Continued) Page 3.6. Conclusion............................................................................... 94 4. Bibliography.................................................................................. 95 5. Appendices................................................................................... 105

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This study focuses on one widespread characteristic of poor soil quality: hydrophobic soil. Previous research has produced . 2.4.1 Comparison of Capillary Rise Method (CRM), moisture content, and .. services (Powlson et al., 2011), such as surface water contamination from agrochemical runoff in
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