Soil water infiltration observation with microwave radiometers
نویسندگان
چکیده
Experiments were conducted using truck-based microwave radiometers operating at 1.41(L-band) and 2.65-GHz (S-band) horizontal polarization to observe small plots during and following sprinkler irrigation. These experiments were conducted on a sandy loam soil in 1994 and a silt loam in 1995. Sandy loam soils typically have higher infiltration capabilities than clays, and in our studies, we were not able to exceed this with the irrigation system. The observed brightness temperature (TB ) quickly reached a nominally constant value during irrigation. When the irrigation was stopped, the TB began to increase as drainage took place. Contributing depth-related differences were observed for Land S-band as expected. The irrigation rates in 1995 with the silt loam soil exceeded the saturated conductivity of the soil. During irrigation, the TB values exhibited a phenomenon that had not been previously observed and identified and is associated with coherent interference. The Land S-band exhibited similar patterns but were not identical due to contributing depth. These results suggested the existence of a sharp dielectric boundary (wet over dry soil) that was increasing in depth with time. The temporal description of the wetting front boundary was used with a coherent radiative transfer model to predict TB for Land S-band.
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ورودعنوان ژورنال:
- IEEE Trans. Geoscience and Remote Sensing
دوره 36 شماره
صفحات -
تاریخ انتشار 1998