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Application of Coffee Ground and Woodchip Biochars as a Soil Amendment for Crop Cultivation : 커피 찌꺼기와 우드칩 바이오차가 토양 개량제로서 작물 재배에 미치는 영향

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dc.contributor.advisorKIM, JAE YOUNG-
dc.contributor.authorMAM SARITH-
dc.date.accessioned2022-03-25T00:25:44Z-
dc.date.available2022-03-25T00:25:44Z-
dc.date.issued2021-
dc.identifier.other000000167628-
dc.identifier.urihttps://hdl.handle.net/10371/177430-
dc.identifier.urihttps://dcollection.snu.ac.kr/common/orgView/000000167628ko_KR
dc.description학위논문(박사) -- 서울대학교대학원 : 공과대학 건설환경공학부, 2021.8. KIM, JAE YOUNG.-
dc.description.abstractApplication of Coffee Ground and Woodchip Biochars as a Soil Amendment for Crop Cultivation

Crop wastes and biomass from feedstocks cause significant environmental problems and have negative consequences for humans. If used correctly, biomass residues contain a great deal of energy potential. Most crop wastes, particularly agricultural leftovers, may be transformed to biochar utilizing thermodynamic technologies such as a muffle furnace. The derivation of wastes for useful materials as well as biochars is the key tool to helps in controlling and handling of biomass in the area or sites. Generally, the operator at temperature at 400 ˚C to make biochar with fixed carbon contents ranging 52.45, and 78% respectively. Biochar conductions into soil amendment for improving the physicochemical and biological properties of the soil owing to biochar's high organic carbon content, which increases the amount of nutrients in the soil and activates it as a carbon sequestration agent over time. Biochar, in and of itself, is a nutrient source that may affect soil nutrient stores and bioavailability, as well as the microbial community and the environment. The majority of nitrogen (N) in the agricultural system is absorbed by plants through ammonium (NH4+) or nitrate (NO3‒). Ammonium is released through mineralization process while NO3‒ is a product of nitrification process through NH4+ oxidation. This method has two parts: (i) NH4+ was transformed to nitrate (NO2-) through ammonia-oxidizing bacteria; (ii) NO2 was changed to NO3 via nitrite-oxidizing bacteria. Increased nitrate (NO3) leakage into waterbodies has made nitrogen losses from fertilizer techniques a significant environmental problem across the world in recent years. Nutrient leaching is a concern not just for soil function and plant uptake, but it may also lead to nutrient enrichment and eutrophication in water, both of which are harmful to human health. Human absorption of excess NO3, for example, can cause newborn methemoglobinemia and a variety of malignancies. As a result, eliminating excess inorganic N from soil solutions or waterbodies has major ecological and societal consequences. Much further, various physical, chemical, and biological techniques for regulating inorganic nitrogen in the aqueous phase have been presented, with adsorption utilizing biochar being one of the most popular.
The primary objective of this research was to demonstrate the application of biochar and the effect of long-term exposure to coffee grounds and wood chips biochar on Pak Choi cultivation in sandy loam soil: (1) to investigate the effects of biochar on adsorption (Park M. H. et al., 2019) and desorption of macronutrients (i.e., N) in the aqueous phase; (2) to study the effect of biochar (biochar-soil mixture) on inorganic nitrogen (N) and plant growth production under plot conditions in the soil phase. (3) to investigate the properties of biochars under long-term exposure or aging in soil environment and (4) to verify biochar effects on crop growth and yield in plot experiment. It is also necessary to study the effect of biochar production on NH4+-N and NO3--N adsorption and desorption to quantitatively explain the relative effect of aging biochar (NH4+-N and NO3--N) on Pak Choi Yields. Furthermore, the kinetics model experiment was important in determining the releasing properties after equilibrium, as well as the long-term exposure characteristics of nitrogen were obtained.
The initial pH of soil (6.55) is in a proper range for plant nutrient uptake whereas the initial pH of coffee grounds biochar (CBC), and woodchips biochar (WBC) varied from moderately alkaline to alkaline. CBC and WBC produced similar yields which varied from about 32.49% to 33.93% by weigh, respectively. The percentage of ash content in CBC (2.9%) was lower than ash content in WBC (11.6%), however, its ash contents were in the average ranges. C/N ratio, ranging from about 52 for CBC and 312 for WCB, respectively. CBC and WBC had O/C and H/C ratios close to the recommendation thresholds, indicating well-pyrolysed ranges, enrichment of aromatic structures, and prone to degradation. The CEC of biochars were similar and were in the average ranges while CEC of the initial soil was in suitable for soil to hold and exchange cations in the soil solution, however, main elements in CBC, WBC, and the initial soil were exchangeable Ca, K, Mg, and Na, respectively. The similar strong peaks decreased at ~1,350 cm‒1 and ~1,600 cm‒1 of C=C and ‒COOH for both CBC and WBC were due to carbon condensation. BET specific surface area of biochars of CBC and WBC were large, this showed that SEM of WBC has more chance to enhance exposure of inorganic minerals as it increased in the pore structure comparing to CBC. The Langmuir isotherm model suited the ammonium nitrogen (NH4+-N) adsorption to both CBC and WBC biocahrs better than the Freundlich isotherm model, with higher r2 values. In comparison to CBC, WBC emitted more nitrogen from the surface. The pseudo-first order and pseudo-second order kinetic models fit better NH4+-N and NO3--N adsorption, respectively. As a result, we concluded that both biochar products can be used in situations where NH4+-N adsorption is a problem, while CBC can be used in situations where NO3--N desorption is a problem. However, more study on using biochars to reduce NO3--N pollution is required.
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dc.description.tableofcontentsChapter 1.Introduction 1
1.1. General Overview 1
1.2. Research Objectives 5
1.3. Dissertation structure 7
References 8

Chapter 2.Literature review 12
2.1. Introduction 12
2.2. Biomass for pyrolysis 13
2.3. Pyrolysis 14
2.3.1 Slow pyrolysis 15
2.3.2. Fast pyrolysis 16
2.4. Biochar Manufacturers Physicochemical properties 17
2.4.1. Biochar s Chemical composition 18
2.4.1. Biochars Surface chemical 20
2.4.2. Spectroscopic analysis of biochar 21
2.5. Biochar application 22
2.5.1. Adsorption and desorption of Inorganic N 22
2.5.2. Total soil organic carbon and total nitrogen 25
2.5.3. Leaching Inorganic of N 26
2.6. Knowledge of gaps 27
References 29

Chapter 3.Prediction of the potential advantages of biochars when surplus Nitrogen fertilizer is applied 33

3.1. Introduction 33
3.2. Materials and methods 36
3.2.1. Biochar production 36
3.2.2. Physiochemical properties of CBC, and WBC 36
3.2.3. Physiochemical properties of Initial soil 37
3.2.4. Extractable cations of CBC, WBC, and initial soil 38
3.2.5. FTIR and BET (Brunauer-Emmett-Teller method) 38
3.2.6. Adsorption and desorption of NH4+-N, and NO3--N 38
3.2.6.1. Adsorption isotherm 38
3.2.7. Adsorption and desorption kinetics of NH4+‒N and NO3‒‒N 39
3.2.7.1 Adsorption kinetics 39
3.2.7.2. Desorption kinetics 40
3.2.7.3. Repetitive NH4+-N, and NO3--N extraction 41
3.2.8. Analytical methods 41
3.3. Results and discussion 42
3.3.1. Physiochemical properties of CBC, and WBC 42
3.3.2. Physiochemical properties of initial soil 46
3.3.3. Extractable cations of the initial soil, CBC, and WBC 47
3.3.4. Electrical conductivity of soil salinity 48
3.3.5. FTIR and Scanning Electron Image (SEM) analysis and BET (Brunauer-Emmett-Teller method 50
3.3.5.1. FTIR -Analysis 50
3.3.5.2. Surface area and pore volume of biochar. 51
3.3.5.3. Scanning Electron Image (SEM) analysis 51
3.3.6. Adsorption and desorption NH4+-N, and NO3--N on CBC, WBC, and initial soil 52
3.3.6.1 Adsorption isotherm of NH4-N, and NO3-N 52
3.3.6.2 Adsorption kinetics of NH4+-N and NO3‒-N onto CBC, WBC and initial Soils 55
3.3.6.3 Desorption kinetics of NH4+-N and NO3‒-N onto CBC, WBC and initial Soils 58
Summary 59
Conference 61

Chapter 4. Investigation of the aged biochars on inorganic Nitrogen (N) and plant growth production under plot conditions in the soil phase 67
4.1. Introduction 67
4.2. Materials and methods 71
4.2.1. Plot design and plant growth experimental process 71
4.2.2. Aged biochar production for one, two, and three years 71
4.2.3. Measurement of main elements 72
4.2.3.1. pH of CBC, WBC, and soils 72
4.2.3.2 Soil sampling and measurement of soil organic carbon and total Nitrogen 71
4.2.4. Adsorption and desorption isotherm 73
4.2.5. Adsorption and desorption kinetics 74
4.2.5.1. Adsorption kinetics 74
4.2.5.2 Desorption kinetics 75
4.2.5.3. RepetitiveNH4+-N and NO3+-N extraction 75
4.2.6. Effects of aged CBC and aged WBC on crop yields 75
4.2.7. Analytical methods 76
4.3. Results and discussion 76
4.3.1. Plot design and plant growth experimental process 76
4.3.1.1. Experimental design plot 76
4.3.1.2. Plant material and cultivation 77
4.3.2. pH of aged CBC, aged WBC, and soils application 80
4.3.3. Extractable cations of Ca, K, Mg, and Na in soils on seasonal crop 80
4.3.4. Adsorption isotherms and kinetics 84
4.3.4.1. NOH4+-N Adsorption isotherms on CBC, WBC 84
4.3.4.2. NO3+-N Adsorption isotherm on CBC and WBC 88
4.3.4.3. NH4+-N and NO3+-N adsorption kinetics on aged CBC, WBC soils 88
4.3.4.4. NH4+-N adsorption kinetics on aged CBC 89
4.3.4.5. NH4+-N and NO3+-N adsorption kinetics on aged CBC and WBC 91
4.3.4.6. NH4+-N adsorption kinetics on aged CBC 93
4.3.4.7. NO3+-N adsorption kinetics on aged CBC 95
4.3.4.8. NH4+-N and NO3+-N Adsorption Kinetics onto three years of soil applications 95
4.3.4.9. NH4+-N and NO3+-N Desorption Kinetics onto aged biochars of CBC and WBC
4.3.4.9.1 NH4+-N and NO3+-N desorption kinetics on aged CBC and WBC 103
4.3.5. Effect of aged biochars on Pak Choi Growth 104
Summary 106
References 107

Chapter 5.Investigation of the property change of biochars and microbiology under long-term exposure in the soil environment 110

5.1. Introduction 110
5.2. Materials and methods 112
5.2.1. Experimental design and sampling 112
5.2.2. Biochar production and propertis 112
5.2.3. Physiochemical properties of CBC, WBC 112
5.2.4. Soil anlysis 113
5.2.5. Extraction of genomic DNA and mRNA (or DNA extraction and sequencing) 114
5.2.6. Analytical methods 114
5.3. Results and discussion 115
5.3.1. Effects of coffee ground and woodchip biochar on soil organic carbon (SOC) conten, total nitrogen(TN), and C:N ratio 116
5.3.2. Soil organic carbon (SO) 116
5.3.3. Total Nitrogen (TN) 118
5.3.4. Soil carbon/Nitrogen (C/N) ratio 119
5.4. Biochar production 121
5.4.1. Physiochemical properties of CBC and WBC 121
5.4.2. Biochar surface area and pore volume 125
5.4.3. Bacteria and Fungal Sequencing Data 1206
5.4.4. Composition, riches and diversity of bacterial community 127
References 130

Chapter 6 Conclusion 132
Appendix A 135
Appendix B 143
Appendix C 149
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dc.format.extentxvi, 176-
dc.language.isoeng-
dc.publisher서울대학교 대학원-
dc.subjectBiohcars-
dc.subjectCoffee Ground-
dc.subjectHeavy Metal-
dc.subjectNH4+-N-
dc.subjectNO3--N-
dc.subjectMicrobial Community-
dc.subjectPyrolysis-
dc.subjectWoodchip-
dc.subject.ddc624-
dc.titleApplication of Coffee Ground and Woodchip Biochars as a Soil Amendment for Crop Cultivation-
dc.title.alternative커피 찌꺼기와 우드칩 바이오차가 토양 개량제로서 작물 재배에 미치는 영향-
dc.typeThesis-
dc.typeDissertation-
dc.contributor.AlternativeAuthor사리스-
dc.contributor.department공과대학 건설환경공학부-
dc.description.degree박사-
dc.date.awarded2021-08-
dc.identifier.uciI804:11032-000000167628-
dc.identifier.holdings000000000046▲000000000053▲000000167628▲-
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