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Official Journal of the Asia Oceania Geosciences Society (AOGS)

Table 1 The values of parameter setting of the RRI model used in the study

From: Identification of the spatio-temporal and fluvial-pluvial sources of flood inundation in the Lower Mekong Basin

Parameters

Symbol

Unit

Mountains

Plains

Manning’s coefficient for slope

n

(m−1/3 s)

0.4

0.015

Soil depth

d

(m)

1.0

–

Lateral saturated hydraulic conductivity

ka

(m/s)

0.1

–

Parameter of unsaturated hydraulic conductivity

β

–

9.0

–

Vertical hydraulic conductivity

kv

(cm/h)

–

0.06

Soil porosity

φ

–

–

0.6

Wetting front soil suction head

Sf

–

–

0.273

Manning’s coefficient for river

nriver

(m−1/3 s)

0.03