Landscape complexity and soil moisture variation in south Georgia, USA, for remote sensing applications

被引:7
作者
Giraldo, Mario A. [1 ,5 ]
Bosch, David [2 ]
Madden, Marguerite [1 ]
Usery, Lynn [3 ]
Kvien, Craig [4 ]
机构
[1] Univ Georgia, Dept Geog, Ctr Remote Sensing & Mapping Sci CRMS, Athens, GA 30602 USA
[2] USDA ARS, SE Watershed Res Lab, Tifton, GA 31793 USA
[3] US Geol Survey, Ctr Excellence Geospatial Informat Sci, Rolla, MO 65401 USA
[4] NESPAL UGA, Coastal Plain Expt Stn, Tifton, GA 31794 USA
[5] Kennesaw State Univ, Dept Geog, Atlanta, GA 30144 USA
基金
美国农业部;
关键词
spatio-temporal analysis; soil moisture; remote sensing; landscape ecology;
D O I
10.1016/j.jhydrol.2008.05.029
中图分类号
TU [建筑科学];
学科分类号
0813 ;
摘要
This research addressed the temporal and spatial variation of soil moisture (SM) in a heterogeneous landscape. The research objective was to investigate soil moisture variation in eight homogeneous 30 by 30 m plots, similar to the pixel size of a Landsat Thematic Mapper (TM) or Enhanced Thematic Mapper plus (ETM+) image. The plots were adjacent to eight stations of an in situ soil moisture network operated by the United States Department of Agriculture-Agriculture Research Service USDA-ARS in Tifton, GA. We also studied five adjacent agricultural fields to examine the effect of different landuses/land covers (LULC) (grass, orchard, peanuts, cotton and bare soil) on the temporal and spatial variation of soil moisture. Soil moisture field data were collected on eight occasions throughout 2005 and January 2006 to establish comparisons within and among eight homogeneous plots. Consistently throughout time, analysis of variance (ANOVA) showed high variation in the soil moisture behavior among the plots and high homogeneity in the soil moisture behavior within them. A precipitation analysis for the eight sampling dates throughout the year 2005 showed similar rainfall conditions for the eight study plots. Therefore, soil moisture variation among locations was explained by in situ local conditions. Temporal stability geostatistical analysis showed that soil moisture has high temporal stability within the small plots and that a single point reading can be used to monitor soil moisture status for the plot within a maximum 3% volume/volume (v/v) soil moisture variation. Similarly, t-statistic analysis showed that soil moisture status in the upper soil layer changes within 24 h. We found statistical differences in the soil moisture between the different LULC in the agricultural fields as well as statistical differences between these fields and the adjacent 30 by 30 m plots. From this analysis, it was demonstrated that spatial proximity is not enough to produce similar soil moisture, since t-test's among adjacent plots with different LULCs showed significant differences. These results confirm that a remote sensing approach that considers homogeneous LULC landscape fragments can be used to identify landscape units of similar soil moisture behavior under heterogeneous landscapes. In addition, the in situ USDA-ARS network wilt serve better in remote sensing studies in which sensors with fine spatial resolution are evaluated. This study is a first step towards identifying landscape units that can be monitored using the single point reading of the USDA-ARS stations network. (c) 2008 Elsevier B.V. All rights reserved.
引用
收藏
页码:405 / 420
页数:16
相关论文
共 30 条
[1]   Upscaling ground observations of vegetation water content, canopy height, and leaf area index during SMEX02 using aircraft and Landsat imagery [J].
Anderson, MC ;
Neale, CMU ;
Li, F ;
Norman, JM ;
Kustas, WP ;
Jayanthi, H ;
Chavez, J .
REMOTE SENSING OF ENVIRONMENT, 2004, 92 (04) :447-464
[2]   Soil moisture estimates from TRMM Microwave Imager observations over the Southern United States [J].
Bindlish, R ;
Jackson, TJ ;
Wood, E ;
Gao, HL ;
Starks, P ;
Bosch, D ;
Lakshmi, V .
REMOTE SENSING OF ENVIRONMENT, 2003, 85 (04) :507-515
[3]   Precipitation, soil moisture, and climate database, little river experimental watershed, georgia, united states [J].
Bosch, D. D. ;
Sheridan, J. M. ;
Marshall, L. K. .
WATER RESOURCES RESEARCH, 2007, 43 (09)
[4]   Little river experimental watershed database [J].
Bosch, D. D. ;
Sheridan, J. M. ;
Lowrance, R. R. ;
Hubbard, R. K. ;
Strickland, T. C. ;
Feyereisen, G. W. ;
Sullivan, D. G. .
WATER RESOURCES RESEARCH, 2007, 43 (09)
[5]   Large scale measurements of soil moisture for validation of remotely sensed data: Georgia soil moisture experiment of 2003 [J].
Bosch, DD ;
Lakshmi, V ;
Jackson, TJ ;
Choi, M ;
Jacobs, JM .
JOURNAL OF HYDROLOGY, 2006, 323 (1-4) :120-137
[6]  
Bosch DD, 2004, T ASAE, V47, P1493, DOI 10.13031/2013.17629
[7]   DIELECTRIC-PROPERTIES AND INFLUENCE OF CONDUCTIVITY IN SOILS AT ONE TO 50 MEGAHERTZ [J].
CAMPBELL, JE .
SOIL SCIENCE SOCIETY OF AMERICA JOURNAL, 1990, 54 (02) :332-341
[8]  
CANGELOSI V, 1976, BASIC STAT REAL WORL, P227
[9]   AN INTERPRETATION OF METHODOLOGIES FOR INDIRECT MEASUREMENT OF SOIL-WATER CONTENT [J].
CARLSON, TN ;
GILLIES, RR ;
SCHMUGGE, TJ .
AGRICULTURAL AND FOREST METEOROLOGY, 1995, 77 (3-4) :191-205
[10]   Microwave remote sensing of soil moisture: Evaluation of the TRMM microwave imager (TMI) satellite for the Little River Watershed Tifton, Georgia [J].
Cashion, J ;
Lakshmi, V ;
Bosch, D ;
Jackson, TJ .
JOURNAL OF HYDROLOGY, 2005, 307 (1-4) :242-253