File:Carbon storage under Miscanthus x giganteus plantations.jpg
From Wikimedia Commons, the free media repository
Jump to navigation
Jump to search
Size of this preview: 538 × 600 pixels. Other resolutions: 215 × 240 pixels | 431 × 480 pixels | 689 × 768 pixels | 919 × 1,024 pixels | 1,851 × 2,063 pixels.
Original file (1,851 × 2,063 pixels, file size: 1.03 MB, MIME type: image/jpeg)
File information
Structured data
Captions
This image was uploaded in the JPEG format even though it consists of non-photographic data. This information could be stored more efficiently or accurately in the PNG or SVG format. If possible, please upload a PNG or SVG version of this image without compression artifacts, derived from a non-JPEG source (or with existing artifacts removed). After doing so, please tag the JPEG version with {{Superseded|NewImage.ext}} and remove this tag. This tag should not be applied to photographs or scans. If this image is a diagram or other image suitable for vectorisation, please tag this image with {{Convert to SVG}} instead of {{BadJPEG}}. If not suitable for vectorisation, use {{Convert to PNG}}. For more information, see {{BadJPEG}}. |
Summary
[edit]DescriptionCarbon storage under Miscanthus x giganteus plantations.jpg |
English: Schematic representation of total soil organic C (carbon) and C4-C changes in topsoil after conversion of former C3 cropland (a) or C3 grassland (b) to Miscanthus. The green color of soil organic C represents the contribution of Miscanthus-derived C4-C, and the brown color represents the C derived from C3 cropland or grassland. The yellow circle shows the mean resident time of soil organic matter under Miscanthus, which was around 60 years. T0 represents the starting point of land-use change to Miscanthus. Although Miscanthus roots can penetrate down to 3 m depth, the main root mass of Miscanthus is concentrated within the upper 60 cm. Root growth in the Bsw horizon of our loamy Gleyic Cambisol was restricted because of the oxygen limitation. Accordingly, C4‐C decreased markedly below 50 cm compared to the topsoil (Fig. 1). Nonetheless, up to 33% of total Miscanthus‐derived C accumulated below 50 cm after 21 years. |
Date | |
Source | https://onlinelibrary.wiley.com/doi/full/10.1111/gcbb.12485 |
Author | Huadong Zang, Evgenia Blagodatskaya, Yuan Wen, Xingliang Xu, Jens Dyckmans, Yakov Kuzyakov |
Licensing
[edit]This file is licensed under the Creative Commons Attribution 4.0 International license.
- You are free:
- to share – to copy, distribute and transmit the work
- to remix – to adapt the work
- Under the following conditions:
- attribution – You must give appropriate credit, provide a link to the license, and indicate if changes were made. You may do so in any reasonable manner, but not in any way that suggests the licensor endorses you or your use.
File history
Click on a date/time to view the file as it appeared at that time.
Date/Time | Thumbnail | Dimensions | User | Comment | |
---|---|---|---|---|---|
current | 13:42, 8 June 2021 | 1,851 × 2,063 (1.03 MB) | The Perennial Hugger (talk | contribs) | Uploaded a work by Huadong Zang, Evgenia Blagodatskaya, Yuan Wen, Xingliang Xu, Jens Dyckmans, Yakov Kuzyakov from https://onlinelibrary.wiley.com/doi/full/10.1111/gcbb.12485 with UploadWizard |
You cannot overwrite this file.
File usage on Commons
There are no pages that use this file.
File usage on other wikis
The following other wikis use this file:
- Usage on en.wikipedia.org