Full text: Proceedings, XXth congress (Part 7)

  
International Archives of the Photogrammetry, Remote Sensing and Spatial Information Sciences, Vol XXXV, Part B7. Istanbul 2004 
Physical-based studies have shown that shortwave infrared 
(SWIR) (1400-2500 nm) is strongly influenced by the water 
in plant tissue (Gausman, 1984). In particular, the 
wavelengths at 1530 and 1720 nm seem to be most 
appropriate for assessing vegetation water (Fourty & Baret, 
1998). The water fills out the cavities, forming a more liquid 
environment inside the leaf. With this, occurs a decreasing of 
the differences of the refraction index between the air and the 
hydrated cell wall, which increases its transmittance and 
decreases the reflectance (Moreira, 2001). Therefore the here 
shown results express, inter alia, mainly the differences in 
plant water content for the four pastures. This leads to the 
assumption that vegetal water content, which is linked to 
productivity, is responsible for the second highest correlation 
coefficient between reflectance spectra and SOC. 
4. CONCLUSIONS 
Due to the urge of reliable, fast and inexpensive SOC 
estimation in accordance with environmental politics as the 
Kyoto Protocol, the study evaluated the potential of orbital 
remote sensing for this purpose. 
It was observed a good correlation (r = 0,97) between SOC 
and LAI. Several studies point out, that the LAI can be 
calculated in satellite images by the NDVI (e.g. Friedl, 1997). 
Under this assumption, the good correlation between SOC 
and LAI leads to the promising approach to estimate current 
and potential SOC by remotely sensed LAI determination. 
Furthermore was identified an also good correlation between 
SOC and some spectra of pasture reflectance. A regression 
analysis showed particularly good correlations in the red (r = 
0,96) and shortwave infrared 1 (r = 0,95) spectra. The red 
spectrum refers mainly to photosynthesis activity and the 
SWIR I spectrum to waterleaf content of the pastures. The 
good correlations in these two spectra with SOC lead to the 
conclusion, that photosynthesis activity and  waterleaf 
content, that are detectable by orbital remote sensing, can be 
linked to SOC. It is of interest to investigate these three 
shown correlations of LAI, red and SWIR I spectrum in 
relation to SOC in time and space under similar and different 
circumstances to verify its validation and study the 
possibilities of its applicability for different pasture or other 
land use settings. 
REFERENCES 
Asner, G.P., 1998. Biophysical and biochemical sources of 
variability in canopy reflectance. Remote Sensing of 
Environment, (64)3, pp. 234-253. 
Broge, N.H.; Leblanc, E., 2001. Comparing prediction power 
and stability of broadband and hyperspectral vegetation 
indices for estimation of green leaf area index and 
canopy chlorophyll density. Remote Sensing of 
Environment, (76,)2, pp. 156-172. 
Escola Superior de Agricultura “Luiz de Queiroz” 
(ESALQ/USP) Base de dados da estagdo meteorologica 
automatizada. http://ce.esalq.usp.br/dce/postoaut.htm (28 
Aug. 2003). 
Fourty, T.; Baret, F, 1998. On spectral estimates of fresh leaf 
biochemistry. /nternational Journal of Remote Sensing, 
(19)7, pp. 1283-1297. 
Friedl, M.A., 1997. Examining the effects of sensor 
resolution and sub-pixel heterogeneity on spectral 
vegetation indices: Implications for biophysical 
modeling. In: Scale in remote sensing and GIS. Boca 
Raton: Lewis Publications, pp.125-139. 
Gausman, H.W.; Burke, J.J.; Quisenberry, J.E., 1984, Use of 
leaf optical-properties in plant stress research. ACS 
Symposium Series, (257), pp. 215-233. 
Henderson, T.L.; Szilagyi, A.; Baumgardner, M.F.; Chen, 
C.C.T. & Landgrebe, D.A, 1989 Spectral band 
selection for classification of soil organic-matter content. 
Soil Science Society of America Journal, (53)6, pp. 
1778-1784. 
Hodgson, 1.G., 1990. Grazing management — science into 
practice. Longman Scientific and Technical, Essex, 
203p. 
Intergovernmental Panel On Climate Change (IPCC), 2000. 
Land use, land-use change, and forestry special report. 
Cambridge: IPCC. 
Markham, B.L.; Barker, J.L., 1986. Landsat MSS and TM 
postcallibration on dynamic ranges of exoatmospheric 
reflectances and at satellite temperatures. EOSAT 
(Landsat Technical Notes, 1), Lanham. 
Major, D.J.; Janzen, H.H.; Olson, B.M.; Mc Ginn, S.M., 
1992. Reflectance characteristics of Southern Alberta 
soils. Canadian Journal Of Soil Science, (72)4, pp. 611- 
615. 
Moreira, M.A., 2001. Fundamentos do sensoriamento remoto 
e metodologias de aplicacáo. Com Deus, Sào José dos 
Campos. 
NASA. Landsat 7 science data users handbook. chapterll. 
http://Itpwww.gsfc.nasa.gov/LAS/handbook/handbook h 
tmIs/chapterl l/chapterl 1.html. (03.02.2003). 
Trimble Navigation Limited., 1999. Characterizing accuracy 
of Trimble Pathfinder mapping receivers. 
US Geological Survey (USGS) 1999, Landsat 7 Datasets 
Document. 
http://eosims.cr.usgs.gov:5725/DATASET/landsat? 
dataset.html (accessed 03 Feb. 2003). 
Walsh, M.J., 1999. Maximizing financial support for 
biodiversity in the emerging Kyoto protocol markets. 
The Science of the Environment, (240), pp. 145-156. 
ACKNOWLEDGEMENTS 
The authors thank for the research support, provided by 
Conselho Nacional de Desenvolvimento Científico, Brazil 
(CNPq) with Grant No. 133344-2000-2 and financial support 
by the Institut de Recherche pour le Développement (IRD), 
France. 
Al 
0Z( 
TS. 
The 
mo 
car 
me; 
rem 
ord 
abs 
196 
alw 
per 
gen 
abs 
bef 
finc 
exp 
on 
Ver 
imp 
the 
Ox 
atm 
qua 
the 
con 
env 
the 
stro 
Stro 
rem 
mes 
Maj 
(Mc 
thes 
fror 
dep 
this 
indi 
(Ba 
goa 
fore
	        
Waiting...

Note to user

Dear user,

In response to current developments in the web technology used by the Goobi viewer, the software no longer supports your browser.

Please use one of the following browsers to display this page correctly.

Thank you.