Incorporation of spatial autocorrelation improves soil-landforming at A and B horizons
The result's identifiers
Result code in IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00025798%3A_____%2F19%3A00000286" target="_blank" >RIV/00025798:_____/19:00000286 - isvavai.cz</a>
Result on the web
<a href="https://www.sciencedirect.com/science/article/pii/S0341816219303686?via%3Dihub" target="_blank" >https://www.sciencedirect.com/science/article/pii/S0341816219303686?via%3Dihub</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.1016/j.catena.2019.104226" target="_blank" >10.1016/j.catena.2019.104226</a>
Alternative languages
Result language
angličtina
Original language name
Incorporation of spatial autocorrelation improves soil-landforming at A and B horizons
Original language description
Research has shown that the performance of soil–landform models would improve if the effects of spatial autocorrelationwere properly accounted for; however, it remains elusive whether the level of improvement wouldbe predictable, based on the degree of spatial autocorrelation in the model variables. We evaluated this problemusing 11 soil variables acquired from the A and B horizons along a hillslope of Žofínský Prales in the CzechRepublic. The results showed that, with no exception, there were increases in R2 and decreases in the Akaikeinformation criterion (AIC), residual autocorrelation, and root-mean-square errors (RMSEs), after incorporatingthe spatial filters extracted by spatial eigenvector mapping into non-spatial regression models. Furthermore, theimprovement of the model was positively proportional to the degree of spatial autocorrelation, inherent in thesoil variables. That is, there were strikingly linear and significant relationships, in which strongly autocorrelatedsoil variables (i.e., having a high Moran's I value) exhibited greater increases in R2 and decreases in AIC, residualautocorrelation, and RMSEs than their more weakly autocorrelated counterparts. These findings indicate that thedegree of spatial autocorrelation present in soil properties can serve as a direct indicator for how much theperformance of a traditional non-spatial soil–landform model would be enhanced, by explicitly taking intoconsideration the presence of spatial autocorrelation. More generally, our results potentially imply that the needfor and benefit from incorporating spatial effects in geopedological modeling proportionally increases as the soilproperty of interest is more spatially structured (i.e., landform variables alone cannot capture soil spatialvariability).
Czech name
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Czech description
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Classification
Type
J<sub>imp</sub> - Article in a specialist periodical, which is included in the Web of Science database
CEP classification
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OECD FORD branch
40104 - Soil science
Result continuities
Project
<a href="/en/project/GA18-17295S" target="_blank" >GA18-17295S: Climate and air pollution effects on forest productivity</a><br>
Continuities
P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)
Others
Publication year
2019
Confidentiality
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Data specific for result type
Name of the periodical
Catena
ISSN
0341-8162
e-ISSN
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Volume of the periodical
183
Issue of the periodical within the volume
December :104226
Country of publishing house
DE - GERMANY
Number of pages
14
Pages from-to
nestránkováno
UT code for WoS article
000488417700043
EID of the result in the Scopus database
2-s2.0-85071738525