\u00a9 shutterstock\/VectorMine<\/figcaption><\/figure>\n\u201cThe big takeaway from the new study is that most of the things we thought we knew about soil carbon were wrong,\u201d said Kate Heckman of the U.S. Forest Service, who led the research.<\/p>\n
\u201cOur initial hypothesis centred on the importance of certain kinds of soil minerals that we assumed were important in carbon persistence, or how long carbon stays in soil. We also thought that temperature patterns across the sites would be a strong regulator of carbon age, but we didn\u2019t see the signals we expected to see associated with either temperature or soil mineralogy.\u201d<\/p>\n
The researchers analysed samples to understand how the ecosystem is changing<\/h3>\n
The Oregon State team and collaborators from Virginia Tech, Michigan Tech, the University of Colorado, and the Pacific Northwest National Laboratory looked at 400 soil core samples from 34 sites. The cores provide an understanding of thousands of layers of soil, which show different characteristics based on age and composition.<\/p>\n
\u201cOpening the cores was like seeing different parts of the country through an eight-by-200-millimetre soil snapshot,\u201d said Adrian Gallo, who performed many of the initial core analyses as a doctoral student under Hatten. \u201cIt was not uncommon to open up the cores and think, \u2018What on Earth is happening here with the colours and rocks and roots?\u2019 And then I\u2019d have to look at aerial imagery, topography maps, and soil descriptors from nearby locations to help me understand the landscape history.\u201d<\/p>\n
\u201cOur results show that when predicting the response of soil carbon to climate change, particularly at a site in a dry ecosystem, we need to consider the history of climate and soil on that site,\u201d Hatten added.<\/p>\n
Radiocarbon and molecular composition analyses on the core samples were performed by the researchers to highlight the relationship between the abundance and persistence of carbon sequestered in the soil and the availability of moisture.<\/p>\n
The scientists divided the core sample sites into being from areas that could be broadly described as either having a humid or arid climate. The division is associated with differences in organic carbon decomposition rates from site to site.<\/p>\n
\u201cSoil organic carbon is being considered as one of the more promising carbon sequestration approaches we have, and understanding the role moisture plays in that process is critical to helping us realise that potential,\u201d Heckman said.<\/p>\n
\u201cMy hope is that this study encourages a lot of our science community to examine the role of moisture in the terrestrial carbon cycle.\u201d<\/p>\n","protected":false},"excerpt":{"rendered":"
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