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В.В. Дикусар, С.В. Засухин

54

ISSN 1812-3368. Вестник МГТУ им. Н.Э. Баумана. Сер. Естественные науки. 2016. № 6

Засухин Сергей Владимирович

— аспирант Московского физико-технического инсти-

тута (государственного университета) (Российская Федерация, 141700, Московская обл.,

Долгопрудный, Институтский переулок, д. 9).

Просьба ссылаться на эту статью следующим образом:

Дикусар В.В., Засухин С.В. Применение быстрого автоматического дифференцирования

при нахождении испарения с поверхности почвы // Вестник МГТУ им. Н.Э. Баумана.

Сер. Естественные науки. 2016. № 6. C. 42–55. DOI: 10.18698/1812-3368-2016-6-42-55

APPLICATION OF FAST AUTOMATIC DIFFERENTIATION

IN THE SOIL SURFACE EVAPORATION PROBLEM

V.V. Dikusar

1

dikussar@yandex.ru

S.V. Zasukhin

2

s.zasukhin@yandex.ru

1

Dorodnitsyn Computing Centre, Federal Research Centre Computer Science

and Control, Russian Academy of Sciences, Moscow, Russian Federation

2

Moscow Institute of Physics and Technology (State University), Dolgoprudny,

Moscow Region, Russian Federation

Abstract

Keywords

Evaporation from the soil surface is an important and often

hard-determined part of modeling the vertical water transfer

in soil. The study considers the problem of determining

evaporation and formulates it as an optimal control prob-

lem. The objective function is mean-square deviation of

modeled values of soil moisture at various depths from some

prescribed values. We found the numerical solution by the

steepest descent method, and we calculated the gradient of

the objective function by formulas of fast automatic differ-

entiation (FAD). Moreover, we applied FAD method to

estimate the sensitivity of soil moisture at various depths to

changes of evaporation. The findings of the research made it

possible to determine the effective subsurface soil layer in

which it is advisable to compute the objective function.

Numerical results showed that this subsurface soil layer

determination has accelerated the convergence of finding

solutions process and has reduced its run time

Vertical water transfer in soil,

objective function, steepest descent

method, fast automatic differentia-

tion method

REFERENCES

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[2] Van Genuchten

M.Th .

A closed form equation for predicting the hydraulic conductivity of

unsaturated soils.

Soil. Sci. Soc. Am. J

., 1980, vol. 44, pp. 892–898.

[3] Samarskiy A.A. Vvedenie v teoriyu raznostnykh skhem [Introduction to the theory of dif-

ference schemes]. Moscow, Nayka Publ., 1971.