• 検索結果がありません。

Shallow-groundwater-temperature-fluctuations near the water table in the paddy fields showed by the fourier series-香川大学学術情報リポジトリ

N/A
N/A
Protected

Academic year: 2021

シェア "Shallow-groundwater-temperature-fluctuations near the water table in the paddy fields showed by the fourier series-香川大学学術情報リポジトリ"

Copied!
6
0
0

読み込み中.... (全文を見る)

全文

Loading

Table  1  Values of  the FOURIER  coefficients as calculated by  Eqs. (8) to (19).  We  used  these  values to obtain the theoretical values of  G.T
Fig.  4..  Theoretical values (open circles) and the observed values (crosses)  of G..T
Table 2  The values of  EM%=,   i in  and  for AR, AL and Aw during 1965,1966 and 1967

参照

関連したドキュメント

[18] , On nontrivial solutions of some homogeneous boundary value problems for the multidi- mensional hyperbolic Euler-Poisson-Darboux equation in an unbounded domain,

Since the boundary integral equation is Fredholm, the solvability theorem follows from the uniqueness theorem, which is ensured for the Neumann problem in the case of the

We present sufficient conditions for the existence of solutions to Neu- mann and periodic boundary-value problems for some class of quasilinear ordinary differential equations.. We

“Breuil-M´ezard conjecture and modularity lifting for potentially semistable deformations after

Then it follows immediately from a suitable version of “Hensel’s Lemma” [cf., e.g., the argument of [4], Lemma 2.1] that S may be obtained, as the notation suggests, as the m A

MEHMET AL SARIG ¨ OL Department of Mathematics, Pamukkale University, 20017 Denizli, Turkey e-mail

Zhang; Blow-up of solutions to the periodic modified Camassa-Holm equation with varying linear dispersion, Discrete Contin. Wang; Blow-up of solutions to the periodic

Due to Kondratiev [12], one of the appropriate functional spaces for the boundary value problems of the type (1.4) are the weighted Sobolev space V β l,2.. Such spaces can be defined