Dagurov(P.N.,(Chimitdorzhiev(T.N.( dpn@ipms.bscnet.ru( ( ( - - PowerPoint PPT Presentation

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Dagurov(P.N.,(Chimitdorzhiev(T.N.( dpn@ipms.bscnet.ru( ( ( - - PowerPoint PPT Presentation

Dagurov(P.N.,(Chimitdorzhiev(T.N.( dpn@ipms.bscnet.ru( ( ( Institute(of(Physical(Material(Science(SB(RAS ! 1! 2! 3! Complex!dielectric!constant!of!moist!soil! ! = ! 1 %! 2% ! ! 1 = ( 2,8620,012 ' +0,001 () + (


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SLIDE 1

Dagurov(P.N.,(Chimitdorzhiev(T.N.(

dpn@ipms.bscnet.ru( (

( Institute(of(Physical(Material(Science(SB(RAS!

1!

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SLIDE 2

2!

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SLIDE 3

3!

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SLIDE 4

!=​!↓1 −%​!↓2% ! ​!↓1 =(2,862−0,012'+0,001()+(3,803+0,462'−0,341()*+(119,006−0,500'+0,633()​ *↑2% ! ​!↓2 =(0,356−0,003'−0,008()+(5,507+0,044'−0,002()*+(17,753−0,313'+0,206()​ *↑2 !

Complex!dielectric!constant!of!moist!soil!

0.1 0.2 0.3 0.4 4 8 12 16 20 24 ε1 w ( ) ε2 w ( ) w

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SLIDE 5

​,↓- =​./01−√⁠!−​(0%31)↑2 /./01+√⁠!−​(0%31)↑2 ! ​,↓5 =​!%./01−√⁠!−​(0%31)↑2 /!%./01+√⁠!−​(0%31 ,=​(​6↓3% +​6↓2 )(​6↓2% −​6↓1 )​7↑%​8↓29 : +(​6↓3% −​6↓1 )(​6↓2% +​6↓1 )​7↑ −%​8↓29 : /(​6↓3% +​6↓2 )(​6↓2% +​6↓1 )​7↑%​8↓29 : +(​6↓3% −​6↓1 )(​6↓2% −​ 6↓1 )​7↑−%​8↓29 : !

Reflection!coefficient!

5!

Homogeneous!soil! Layer!soil!

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SLIDE 6

0! 0.1! 0.2! 0.3!

w!

170! 172! 174! 176! 178! 180!

1 - θ = 0о, 2 - θ = 40о, 3 - θ = 60о!

!!

ϕ,!degree!

1! 3!

2!

6!

!The!argument!of!the!reflection!coefficient!versus! volumetric!moisture!content.!Homogeneous!soil.! !

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SLIDE 7

7!

0! 0.1! 0.2! 0.3!

w!

!!

120! 132! 144! 156! 168! 180!

d = 2 см , λ = 23 cm

1, 2 – moisture content of the layer varies, moisture of the soil is 0.3 and 0.1, respectively; 3, 4 - moisture content of the soil varies, moisture of the layer is 0.3 and 0.1, respectively.! !!

"!

!!

1! 1! 2! 4! 3!

!The!argument!of!the!reflection!coefficient!versus!

volumetric!moisture!content.!Layer!soil.! !

ϕ,!degree!

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SLIDE 8

8!

Thanks!for!your!attention!!

It! is! shown! that! the! layered! structure! of! the! moist! soil! leads! to! significant! changes! in! the! argument! of! the! reflection!coefficient,!reaching!several!tens!of!degrees.!! These! variations! should! be! taken! into! account! in! the! method!of!differential!radar!interferometry!(DInSAR).!

Conclusions!