Abstract
To investigate changes in the nature of soil organic matter with lapse of time after burial, buried humic horizons derived from volcanic ash with an age from the present to 27,200 YBP were studied and the properties of the soil organic matter in each horizon were assessed. The results for the chemical properties and humus composition of the soil samples were as follows. 1) Based on stratigraphical studies (1), the Ashitaka Loam Formation is divided into two groups of alternate layers, Kuroboku soil in the surface part, and the Upper loam below the Kuroboku soil. The total carbon and nitrogen contents were high in the horizons of the Kuroboku soil and low in the Upper loam. The relationship between the total carbon and nitrogen contents had a positive correlation. 2) The humus compositions of the two groups were as follows. (1) Kuroboku soil: This was characterized by large amounts of humic acid extracted with NaOH and small amounts of both humic acid and fulvic acid extracted with Na6P2O7 Compare...
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a callDisclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.
