Abstract

This study evaluated the contribution of small agricultural reservoirs (the mool-tongs) to crop production on Udo, and the role they play. Agricultural water demand and deficit, water storage in the mool-tongs, and the amount of irrigation water were analyzed by applying the water balance model. In particular, the Blaney-Criddle method was used to estimate the agricultural water for crop growth. In this study, four typical crops of garlic, spring onion, peanut, and barley were considered, whose growing seasons were somewhat different from each other. A total of 47 years (1973–2019) of rainfall, temperature, and evaporation data were used in this study. As a result, it was confirmed that the crop coefficient, growing period of a crop, share of the cultivated area, and the seasonal distribution of rainfall affect the role of the mool-tongs. Comparison of the frequencies of occurrence of agricultural water deficit and irrigation interval before and after introducing the mool-tongs also confirms their usefulness. After the introduction of the mool-tongs for irrigation, the frequency of occurrence of agricultural water deficits changed significantly, from almost 30% of the entire simulation period to less than 20%. Even though the water supply capacity of the mool-tongs on Udo is insufficient to offset the entire agricultural water deficit, the water stored in the mool-tongs was found to considerably aid the survival of the crops and increase crop production. The results in this study can help to determine the capacity of rainwater collecting systems, especially on a small island where the available water resources are limited.

Highlights

  • On small islands, it is generally the case that the available water is small

  • The first analysis was performed without considering the mool-tongs, with the results evaluated from the point of crop production

  • The objective of this study was to demonstrate the contribution of mool-tongs to crop production on Udo, and the role they play

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Summary

Introduction

It is generally the case that the available water is small. Water for agricultural use is not easy to collect. The area of the island is too small to collect much surface water, nor is sufficient ground water expected. Island residents are highly vulnerable to drought, and the impact of no rain appears immediately [1]. On volcanic islands, where the infiltration capacity of soil is high, the problem can be more serious. It becomes even more difficult to collect the surface water [2]. Recent climate change has degraded the stability of the water supply, mainly due to the change in rainfall patterns [3,4,5]

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