- Page 1 and 2: Volume I From Molecular Understandi
- Page 3 and 4: Dedication to the memory of Profess
- Page 5 and 6: Organizing Committee Lunin, Valery,
- Page 7 and 8: Preface The 20 th century was the c
- Page 9 and 10: Dear colleagues and friends of humi
- Page 11 and 12: On behalf of the International Unio
- Page 13: On behalf of the Government of Mosc
- Page 17 and 18: High Resolution Ultrasonic Spectros
- Page 19 and 20: Impact on SOM of an Oxisol after Ap
- Page 21 and 22: Characterization of Microbiological
- Page 23 and 24: Size Exclusion Chromatography Inves
- Page 25 and 26: The Influence of Humic Acids on the
- Page 27 and 28: Mitigating Activity of Humic Substa
- Page 29 and 30: Influence of Humic Substances on th
- Page 31: Section I Novel methods and approac
- Page 34 and 35: Reaction Count 3. RESULTS AND DISCU
- Page 36 and 37: Assuming that bacteria can only uti
- Page 38 and 39: pH a spin probe with appropriate pK
- Page 40 and 41: ACKNOWLEDGEMENTS This work was supp
- Page 42 and 43: employing the high resolution ultra
- Page 44 and 45: a degree of humification. It is not
- Page 46 and 47: during their transformation from po
- Page 48 and 49: 8. Kujawinski, E. B.; Hatcher, P. G
- Page 50 and 51: Figure 1. Information transfer in o
- Page 52 and 53: The availability of high-resolution
- Page 54 and 55: 2. MATERIALS AND METHODS Groundwate
- Page 56 and 57: in Fig. 2 were calculated by dividi
- Page 58 and 59: 2. MATERIALS AND METHODS A surface
- Page 60 and 61: 3. Horsfield, B., Disko, U. and Lei
- Page 62 and 63: Complex NOM/HS Sample Small molecul
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REFERENCES 1. Chen, J., X. Zhao, R.
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and inorganic components has been s
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hv-Carbon vs OD-Humin-Carbon p y 1,
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aliquot was withdrawn, the particle
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HA is relatively low, PQ appears to
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Humic acid of the charcoal from sug
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4. CONCLUSIONS UV-Vis spectra show
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until the desired water content was
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Table 1. Comparison of non-freezing
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and recycle delays of 500 ms were u
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A DMSO-concentrated H 2 SO 4 mixtur
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Fig. 1. Topographic change of solid
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REFERENCES 1. Baldock, J.A., Oades,
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different on molecular size (MS) an
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B, C+D. In high MS fraction A a str
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ab-initio single-point calculation
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0~20cm topsoil. With the Pallo meth
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Figure 3. The IR spectra of HMc und
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potential and the ratio of the poly
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The H-binding data can be fitted by
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Table 1. The characteristic of peat
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(CASE) to a comprehensive set of sp
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disks (Varian, Inc.; conditioning w
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Table 1. (A) 1H-NMR integrals of si
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Each of them gives, of course, a sh
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2. MATERIALS AND METHODS 2.1. Mater
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modules (Figure 1C). The modules A1
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extracted with a 40:1 (v:w) water t
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Figure 2. Spectral editing for iden
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Stock solutions of humic fractions
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4. CONCLUSIONS The mobile and recal
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GC/MS and ultrahigh resolution Four
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Figure 3. FT-ICR mass spectrum of T
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increase of ΔN values was observed
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4. CONCLUSIONS Preliminary results
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Figure 1. FTICR Mass-spectra of Ind
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2. MATERIALS AND METHODS The humin
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4. CONCLUSIONS The use of extractio
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then neutralized with 1 M NaOH to p
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the slurry addition with a general
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Electrodialysis (ED) appears as an
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Salinity 45 40 35 30 25 20 15 10 5
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4.60 ± 0.25 and 8.54 ± 0.35. resp
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4. CONCLUSIONS As in soil, the bene
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PRAM characterization was done foll
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evaluation of variability of NOM. T
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Ultrafiltration of HA was carried o
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evealed pale red fluorescence. Frac
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observed between 1 H-NMR spectra of
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HA HAU A B C+D 300 250 200 150 100
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cm 2 /V s and for nHA was (1.36±0.
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Area of region 2 in both cases show
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3. RESULTS AND DISCUSSION 2 1.8 1.6
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products, but to pay attention to t
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small amount of each type of molecu
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Evolution of Soil Humic Substances
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It is exposed to constant biotical
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Humus and the Birth of Pedology : M
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Freshwaters: Do ‘Humics’ Always
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Table 1. Concentration of ROM (expr
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Atmospheric HULIS: How Humic-Like A
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hindrance of water vapor diffusion
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Short Time Humification and Mineral
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C regions we detected a total reduc
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Sedimentary Organic Matter in the E
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increase of temperature, which is t
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Biological and Molecular Structure
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epresenting carbohydrates and ligni
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Genesis of Cambisol, Luvisol and Re
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1 2 3 4 Figure 1. 13 C NMR spectras
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Paramagnetic Activity of Humic Acid
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Global Warming and Effects of Sea-S
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Deposition (mm); Chloride (mg/L) 10
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Characterization of Soil Organic Ma
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Excitation λ (nm) 465 440 420 400
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Soil Organic Matter Chemical and Ph
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Study on the Role of Microorganism
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Figure 1. IR spectrum of HA at diff
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Impact on SOM of an Oxisol after Ap
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Figure 2 shows relative percentage
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Organic Matter in Oxisol Profiles u
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the degree of oxidation decreases i
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Chemical and Spectroscopic Characte
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P-HA E x /E m 340/404 FI 482 E x /E
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Effect of Different Fruit Tree Cult
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content of so called “fulvic frac
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Long-Term Effects of Wildfires in t
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HWOC (% of total OC) 4 0 fires 1 fi
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Organic Carbon Stocks in Bulgarian
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6. Filcheva, E., Rousseva, S., Kuli
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Use of Lipid Biomarkers in Sediment
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3. RESULTS AND DISCUSSION Lipid ext
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Thermal Properties in Soil Particle
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complexes. EP2/EP1 ratios of both p
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Soil Organic Carbon Stocks and Humi
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Forest stand Table 2. Stocks of Car
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Mechanisms of Soil Carbon Storage i
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-26 -27 (a) C3 plots average δ 13
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The Content of Humic Substances in
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The correlation between the value o
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Espectroscopic Features of Humic Su
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for “Ravelo” showing 18.8% (AH)
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Characterization of Humic and Fulvi
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groups and the increment of dissoci
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Distribution of Water Soluble Organ
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espectively. Such distribution was
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Evolution and NOM Kari Hänninen Un
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Long Term Trends of DOC and Colour
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Climatic change towards more freque
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Role of Aromaticity Degree in the S
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ecause some problems may appear whe
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Humic Acids Structure as a Reflecti
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Table. HA/FA and basic structural i
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Bioluminescent Monitoring of Detoxi
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approaching it to control, thus, de
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Humus Substances in Natural and Tec
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mg C L -1 16 12 surface bottom DOC
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Analysis of Pore Water Dissolved Or
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450 HUMIC-LIKE Emission, nm 400 350
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Risk Assessment of Soil Degradation
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P ij - density of possible events d
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Variation in Lipid Relative Abundan
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Characterization of Humic Substance
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Characterization of Soil and Humic
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structure (Figure 2) (7). The HA sa
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Diversity of Fractional Composition
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60 C % 50 40 30 20 10 0 1/Ap 1/ABbr
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Characterization of Microbiological
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Reactive Polyphenols and Dissolved
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DOC (mg/L) 9 8 7 6 5 4 3 Stream Hil
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Density Fractions of SOM in Mediter
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* * * Fatty acids Aromatic compound
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Use of Bioluminescent Assay Systems
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100 Activation stage Inhibition sta
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Humification of Peat and Characteri
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the peat samples mostly show negati
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The Impact of Land Use Conversion o
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Sample Table 2 . MW, D 465 and E 4
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Char and Humin Fractions in Amazoni
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The δ 13 C values of the humic fra
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Diverse Microbial Carbon Turnover a
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After one month, recoveries of trop
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The Comparison between Humus Struct
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Table 2: Humus structure of 5 to 1
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Properties of Humic Acids in Forest
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for soil profiles under angiosperm
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Fluorescence Spectroscopy of Humic
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Synchronous-scan fluorescence spect
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In Situ Humification and Humics Pre
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Comparison of 13 C NMR Spectra of F
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Figure 1. Liquid-state 13 C NMR spe
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Correlation between Optical and Che
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molecular weight and more hydrophob
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Difference between Humic Acids from
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Table 2. Percentages of functional
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Humus Level in Soils of South Kazak
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All results were elaborated statist
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The Role of Lichens in Carbon Prese