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@ARTICLE{Rodionov:823906,
author = {Rodionov, Andrei and Pätzold, Stefan and Welp, Gerhard and
Pude, Ralf and Amelung, Wulf},
title = {{P}roximal field {V}is-{NIR} spectroscopy of soil organic
carbon: {A} solution to clear obstacles related to
vegetation and straw cover},
journal = {Soil $\&$ tillage research},
volume = {163},
issn = {0167-1987},
address = {Amsterdam [u.a.]},
publisher = {Elsevier Science},
reportid = {FZJ-2016-06538},
pages = {89 - 98},
year = {2016},
abstract = {The assessment of soil organic carbon (SOC) content using
proximal diffuse reflectance spectroscopy in the visible and
near-infrared (Vis-NIRS) may be hampered if green plants
(photosynthetic vegetation) and straw (non-photosynthetic
vegetation) are present in the measuring spot. Under such
conditions, taking spectra of the soil surface yields
insufficient results and requires quantitative correction.
In this combined lab and field study, we investigated if,
and to what degree, it is possible to distinguish green
plants and straw from bulk soil organic matter using the
same Vis-NIR spectra. Without any modification of an
approved SOC model, SOC was overestimated by more than
$200\%,$ depending on the fractional coverage with green
leaves and straw. This error was more severe for green
leaves than for straw. After covering the soil surface with
defined proportions of green barley leaves or straw
concomitant changes in reflectance spectra were recorded.
Partial least squares regression (PLSR) with three factors
yielded quantitative predictions of soil coverage by green
leaves (R2adj = 0.98, RMSEcv of cross-validation = $5.3\%$
soil coverage) and straw (R2adj = 0.95, RMSEcv = $7.5\%$
soil coverage). Furthermore, photosynthetic and
non-photosynthetic vegetation indices, the Normalized
Difference Vegetation Index (NDVI) and the Cellulose
Absorption Index (CAI), were derived from the Vis-NIR
spectra of the soil surface. Both indices increased when
covering with green leaves or straw increased (R2 = 0.99
[NDVI] and 0.94 [CAI], respectively). The degree of SOC
overestimation was correlated with NDVI and CAI.
Second-order polynomial regressions between SOC
overestimation, and CAI or NDVI were fitted (R2 = 0.97 and
0.99, respectively). This enabled us to carry out a
correction step after predicting SOC using an approved SOC
model (R2adj = 0.84, RPD = 2.53, RMSECV = 0.73) to minimize
the overestimation error. Transferring this
two-step-approach to field conditions revealed that Vis-NIR
spectra still showed scattered predictions of point-specific
SOC contents (R2 = 0.66 and 0.58 for stop-and-go and
on-the-go acquisitions, respectively), however, with a slope
close to unity. Consequently, the disturbance by green
plants or straw on the soil surface during superficial
Vis-NIR sensing of SOC in the field can be overcome.},
cin = {IBG-3},
ddc = {630},
cid = {I:(DE-Juel1)IBG-3-20101118},
pnm = {255 - Terrestrial Systems: From Observation to Prediction
(POF3-255)},
pid = {G:(DE-HGF)POF3-255},
typ = {PUB:(DE-HGF)16},
UT = {WOS:000381834000011},
doi = {10.1016/j.still.2016.05.008},
url = {https://juser.fz-juelich.de/record/823906},
}