Terra Preta
Thesis about Anthrohumox in Brazilian Lowland
Table of Content
Terra Preta
Natural conditions of the Amazon region and in particular the study area
- 2.1 Geology and morphogenesis
- 2.1.1 Precambrian and Paleozoic
- 2.1.2 Mesozoic
- 2.1.3 Tertiary with Barreiras series and Belterra clay
- 2.1.4 Quarternary with Pleistocene and Holocene
- 2.2 Geomorphology
- 2.3 Climate
- 2.3.1 Amazonia
- 2.3.2 Belterra
- 2.4 Hydrology
- 2.4.1 River typology
- 2.4.2 Suspended matter and nutrient balance
- 2.5 Vegetation
- 2.5.1 Characteristics
- 2.5.2 Production and mineralization of organic matter
- 2.5.3 Nutrient cycle
- 2.5.4 Anthropogenic use
- 2.5.5 Region around Santarém
- 2.6 Soil science: An overview of the tropical soils of Amazonia
- 2.6.1 FAO classification system and mapping
- 2.6.2 7thSoil Approximation and their use in the definition
- 2.6.3 Brazilian soil classification and mapping
- 2.6.4 Other soil classifications
- 2.6.5 Summary description of latosol
- 2.6.6 Other soil types of Amazonia
- 2.7 Population and settlement projects in Amazonia
Field work
Investigation methods
- 4.1 Preparation of samples
- 4.2 Determination of volumetric weight
- 4.3 Determination of maximum water capacity
- 4.4 Determination of particle sizes
- 4.5 Determination of acidity
- 4.6 Outcrop
- 4.6.1 Choice of method
- 4.6.2 Na2CO3 outcrop
- 4.7 Atomic absorption spectroscopy
- 4.7.1 Principle
- 4.7.2 Interference phenomena
- 4.7.3 Measurement
- 4.7.4 Sit measurement
- 4.7.5 Alt measurement
- 4.7.6 Fet measurement
- 4.7.7 Mnt measurement
- 4.7.8 Tit measurement
- 4.7.9 Cat measurement
- 4.7.10 Mgt measurement
- 4.7.11 Kt measurement
- 4.8 Dithionit extraction and measurement
- 4.9 Oxalat extraction and measurement
- 4.10 Color analysis
- 4.11 14C dating
- 4.12 Mineral analysis
Statistical evaluation
- 5.1 Further calculation
- 5.2 Possibility to test the analysis process
- 5.3 Mean value calculation according to depth gradations
- 5.4 Error possibilities and outlier tests
- 5.5 Analysis of variance
- 5.6 Correlation analysis
Presentation of results and discussion
- 6.1 Volumetric weight
- 6.1.1 Results of Latosol
- 6.1.2 Results of TP
- 6.1.3 Comparison Latosol - TP
- 6.1.4 Explanation of values
- 6.1.5 Inhomogeneity of TP
- 6.1.6 Calculation of supply quantity
- 6.1.7 Substance and pore volume
- 6.1.8 Air analysis
- 6.1.9 Consistency
- 6.1.10 Total volumetric weight
- 6.2 Soil water
- 6.2.1 Pore distribution and water tension
- 6.2.2 Ecological relevance
- 6.3 Particle size
- 6.3.1 Results of Latosol
- 6.3.2 Results of TP
- 6.3.3 Comparison Latosol - TP
- 6.3.4 Silt : clay ratio
- 6.3.5 Explanation of high clay content
- 6.3.6 Explanation of higher sand content in topsoil
- 6.3.7 Explanation of higher silt content, especially at depth of 70 cm
- 6.3.8 Explanation of (quantitative) difference
- 6.3.9 Mass loss due to clay leaching
- 6.3.10 Ecological relevance
- 6.4 Mineral finding
- 6.5 Acidity
- 6.5.1 Results of Latosol
- 6.5.2 Results of TP
- 6.5.3 Comparison Latosol - TP
- 6.5.4 Difference in organic topsoil
- 6.5.5 Explanation of (low) pH of latosol
- 6.5.6 Explanation of (increased) pH of the TP
- 6.5.7 Conclusions and interactions with other soil properties
- 6.5.8 Ecological relevance
- 6.5.9 Melioration approaches
- 6.6 Si content
- 6.6.1 Results of Latosol
- 6.6.2 Results of TP
- 6.6.3 Comparison Latosol - TP
- 6.6.4 Binding in minerals and solution
- 6.6.5 Silica solubility
- 6.6.6 Explanation of values and their differences
- 6.6.7 Desilication and its quantification
- 6.6.8 SiO2 : Al2O3 ratio
- 6.6.9 SiO2 : R2O3 ratio
- 6.6.10 Ecological relevance
- 6.7 Al content
- 6.7.1 Results of Latosol
- 6.7.2 Results of TP
- 6.7.3 Comparison Latosol - TP
- 6.7.4 Binding in minerals, solution and new formations
- 6.7.5 Al hydroxide
- 6.7.6 Al+++ ions
- 6.7.7 Solubility and resistance to weathering
- 6.7.8 Explanation of values
- 6.7.9 Dithionit soluble Al
- 6.7.10 Oxalat soluble Al
- 6.7.11 Ecological relevance
- 6.8 Fe content
- 6.8.1 Results of Latosol
- 6.8.2 Results of TP
- 6.8.3 Comparison Latosol - TP
- 6.8.4 Binding in minerals, solution and new formations
- 6.8.5 Fe oxides and hydroxides
- 6.8.6 Solubility
- 6.8.7 Influence of organic matter
- 6.8.8 Explanation of values
- 6.8.9 Dithionit soluble Fe
- 6.8.10 Oxalat soluble Fe
- 6.8.11 Al2O3 : Fe2O3 ratio
- 6.8.12 Ecological relevance
- 6.9 Mn content
- 6.9.1 Results of Latosol
- 6.9.2 Results of TP
- 6.9.3 Comparison Latosol - TP
- 6.9.4 Formation in minerals, solution and Mn oxides
- 6.9.5 Solubility
- 6.9.6 Influence of organic matter
- 6.9.7 Explanation of values
- 6.9.8 Dithionit and Oxalat soluble Mn
- 6.9.9 Ecological relevance
- 6.10 Ca content
- 6.10.1 Results of Latosol
- 6.10.2 Results of TP
- 6.10.3 Comparison Latosol - TP
- 6.10.4 Weathering
- 6.10.5 Relation to exchangeable Ca
- 6.11 Mg content
- 6.11.1 Results of Latosol
- 6.11.2 Results of TP
- 6.11.3 Comparison Latosol - TP
- 6.11.4 Binding forms
- 6.11.5 Relation to exchangeable Mg
- 6.12 K content
- 6.12.1 Result
- 6.12.2 Relation to exchangeable K
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Literature
Illustrations
- TP sites of Rio Trombetas and Rio Jamunda
- TP sites of Lago Grande do Curusi
- TP sites in Brazil
- Geological map of Amazonia
- Geological N-S profile through the Amazon valley near Belterra
- Geological profile of Belterra clay
- Geological profile of Belterra clay in Belterra
- Climate regions of Amazonia
- Annual precipitation in Amazonia
- Annual temperatures in Amazonia
- Climate diagrams of Amazonia
- Climate diagram of Belterra
- Soil map of Amazonia
- TP and Varzea near Santarem
- Plateau laterit at escarpment
- Formation of plateau laterit
- TP sites near Belterra
- Isocarbonale presentation of typical TP
- Isocarbonale presentation of transition of TP locality 1 and 2
- Alleged TP distribution in Belterra acc. to Sampaio
- Sample site 'Chico Alfredo'
- Water tension curves of Latosol and TP
- Indicated substance and pore volumes of topsoil and subsoil in Latosol and TP
- Solubility of various oxide compounds as function of pH
- Depth distribution of Ald : Alt in Latosol and TP
- Depth distribution of Alo : Ald in Latosol and TP
- Stability diagram of Fe++, Fe+++, Goethit and amorph Fe molecules
- Depth distribution of Fed : Fet in Latosol and TP
- Depth distribution of Feo : Fed in Latosol and TP
- Stability diagram of Mn++ and Mn oxides
- Depth distribution of Mnd : Mnt in Latosol and TP
- Depth distribution of Mno : Mnd in Latosol and TP
Tables
- Climate data of Belterra
- Comparison of FAO, 7th Approximation and ORSTOM Classification
- TP sites of Belterra
- Particle size distribution of TP profiles investigated in Brazil
- Mol ratios of Fe and Al to organic matter
- Comparison of total to exchangeable Ca
- Comparison of total to exchangeable Mg
- Comparison of total to exchangeable K
Data volume
Explanations
Sample results of Latosol and Terra Preta
- SP1
- SP2
- SP4
- SP5
- SP6
- SP7
- SP8
- SP9
- SP0
- SL1
- SL2
- SL3
- SL4
- SL5
- SL6
- SL7
Static evaluation: Mean calculation, outlier test, analysis of variance, correlation analysis and graphical depth functions
- C content
- Fine earth volumetric weight
- Total volumetric weight
- Particle sizes (only profiles SP2 and SL5)
- pH values
- Si content
- SiO2 : Al2O3 ratios
- SiO2 : Al2O3 +Fe2O3 ratios
- Al content
- Al2O3 : Fe2O3 ratios
- Pedogenic Al (only profiles SP4 and SP4)
- Fe content
- Pedogenic Fe (only profiles SP4 and SP4)
- Mn content
- Pedogenic Mn (only profiles SP4 and SP4)
- Ti content (only profiles SP4 and SP1)
- Ca content
- Mg content
- K content
- P fractions (only profiles SP4 and SL4)
Depth functions of individual profiles
- C content
- Fine earth volumetric weight
- pH values
- Si content
- Al content
- Fe content
- Mn content
- Ca content
- Mg content
