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Materials Data on NaPO by Materials Project

NaPO crystallizes in the orthorhombic Imma space group. The structure is three-dimensional. Na is bonded in a distorted linear geometry to two equivalent O atoms. Both Na–O bond lengths are 2.44 Å. P is bonded in a distorted square co-planar geometry to four equivalent O atoms. There are two shorter (2.16 Å) and two longer (2.19 Å) P–O bond lengths. O is bonded to two equivalent Na and four equivalent P atoms to form a mixture of corner and edge-sharing ONa2P4 octahedra. The corner-sharing octahedral tilt angles are 0°.

36 MATERIALS SCIENCE↗

Materials Data on NaPO by Materials Project

NaPO crystallizes in the orthorhombic Imma space group. The structure is three-dimensional. Na is bonded in a distorted linear geometry to two equivalent O atoms. Both Na–O bond lengths are 2.31 Å. P is bonded in a linear geometry to two equivalent O atoms. Both P–O bond lengths are 1.83 Å. O is bonded in a distorted rectangular see-saw-like geometry to two equivalent Na and two equivalent P atoms.

36 MATERIALS SCIENCE↗

Validation of Forested Inundation Extent Revealed by L-Band Polarimetric and Interferometric SAR Data

UAVSAR, NASA's airborne Synthetic Aperture Radar (SAR), conducted an extended observational campaign in Central and South America in March 2013, primarily related to volcanic deformations along the Andean Mountain Range but also including a large number of flights studying other scientific phenomena. During this campaign, the L-Band SAR collected data over the Napo River in Ecuador. The objectives of this experiment were to acquire polarimetric and interferometric L-Band SAR data over an inundated tropical forest in Ecuador simultaneously with on-the-ground field work ascertaining the extent of inundation, and to then derive from this data a quantitative estimate for the error in the SAR-derived inundation extent. In this paper, we will first describe the processing and preliminary analysis of the SAR data. The polarimetric SAR data will be classified by land cover and inundation state. The interferometric SAR data will be used to identify those areas where change in inundation extent occurred, and to measure the change in water level between two observations separated by a week. Second, we will describe the collection of the field estimates of inundation, and have preliminary comparisons of inundation extent measured in the field field versus that estimated from the SAR data.

Synthetic Aperture Radar (SAR),↗