Soil salinity, fertility and carbon content, and rice yield of salt-affected paddy with different cultivation period in southwestern coastal area of South Korea

Author(s):  
Hyun-Jin Park ◽  
Bo-Seong Seo ◽  
Young-Jae Jeong ◽  
Hye In Yang ◽  
Se-in Park ◽  
...  
2021 ◽  
Vol 10 (01) ◽  
pp. 16-36
Author(s):  
Laila Khatun ◽  
Muhammad Aslam Ali ◽  
Mahmud Hossain Sumon ◽  
Md. Bazlul Islam ◽  
Fahima Khatun

Water ◽  
2020 ◽  
Vol 12 (4) ◽  
pp. 1103 ◽  
Author(s):  
Dongmin Jang ◽  
Wonkyun Joo ◽  
Chang-Hoo Jeong ◽  
Wonsu Kim ◽  
Sung Park ◽  
...  

Typhoons can often cause inundation in lower coastal cities by inducing strong surges and waves. Being affected by typhoon annually, the coastal cities in South Korea are very vulnerable to typhoons. In 2016, a typhoon ‘CHABA’, with a maximum 10 min sustained wind speed of about 50 m/s and a minimum central pressure of 905 hPa, hit South Korea, suffering tremendous damage. In particular, ‘CHABA’-induced coastal inundation resulted in serious damage to the coastal area of Busan where a lot of high-rise buildings and residential areas are concentrated, and was caused by the combined effect of tide, surge, and wave. The typhoon-induced surge raised sea levels during high tide, and the strong wave with a long period of more than 10 s eventually led to the coastal inundation at the same time. The present research focuses a numerical downscaling considering the effects of tide, surge and wave for coastal inundation induced by Typhoon ‘CHABA’. This downscaling approach applied several numerical models, which are the Weather Research and Forecasting model (WRF) for typhoon simulation, the Finite Volume Community Ocean Model (FVCOM) for tide and surge simulation, and the Simulating WAve Nearshore (SWAN) for wave simulation. In a domain covering the Korean Peninsula, typhoon-induced surges and waves were simulated applying the results simulated by WRF as meteorological conditions. In the downscaled domain ranged near the coastal area of Busan, the coastal inundation was simulated blending a storm tide height and an irregular wave height obtained from the domain, in which each height has 1 s interval. The irregular wave height was calculated using the significant wave height and peak period. Through this downscaling study, the impact of storm tide and wave on coastal inundation was estimated.


2019 ◽  
Vol 40 (6) ◽  
pp. 599-605
Author(s):  
Jina Hur ◽  
Kyo-Moon Shim ◽  
Yongseok Kim ◽  
Kee-Kyung Kang

2005 ◽  
Vol 19 (6) ◽  
pp. 1261-1276 ◽  
Author(s):  
Ji-Hoon Kim ◽  
Rak-Hyeon Kim ◽  
Jeongho Lee ◽  
Tae-Jin Cheong ◽  
Byoung-Woo Yum ◽  
...  

2018 ◽  
Vol 29 (10) ◽  
pp. 3772-3782 ◽  
Author(s):  
Wenquan Liu ◽  
Xingyong Xu ◽  
Fang Lu ◽  
Jianrong Cao ◽  
Ping Li ◽  
...  

Akta Agrosia ◽  
2020 ◽  
Vol 23 (2) ◽  
pp. 47-54
Author(s):  
Rustikawati Rustikawati ◽  
Catur Herison ◽  
Muhammad Chozin ◽  
Indres Indres

Coastal area of Bengkulu Province is home of many heirloom rice varieties and play an important role in contributing rice production in the province. However, as the climate change proceeds, a progressive sea water inundation has increased soil salinity mainly in low-lying areas and jeopardizing the sustainability of rice production in coastal regions.  The use of salt-tolerant varieties, therefore, would be a sensible solution to alleviate the adverse effect of soil salinity in respect of maintaining the crop production in the coastal areas. The objective of this study was to examine the salinity tolerance of 20 heirloom rice varieties collected from a coastal area of Bengkulu Province.  Prior to the screening process, lethal concentration 90 (LC90) was determined by assaying the seedlings of ‘Kuning Tinggi’ in a series of nutrient solution containing a different concentration of NaCl (0, 2000, 4000, 6000, 8000 and 10000 ppm). Using a regression analysis, LC90 was detected at a concentration of 3910 ppm. The screening was performed by exposing the varieties in the nutrient solution culture containing 4000 ppm NaCl and growing them on the tidal swamp. Under nutrient culture evaluation, the symptom of NaCl toxicity was scored and converted to salinity tolerance index. ‘Humbur’, ‘Kuning Tinggi’ and ‘Padang Bakung’ exhibited medium tolerant, while ‘Beram’, ‘Imperata’ and ‘Kuning’ exhibited very sensitive. Further evaluation of the tidal swamp for vegetative and generative performances signified that ‘Humbur’ and ‘Kuning Tinggi’ had medium tolerant to salinity stress


2013 ◽  
Vol 10 (2) ◽  
pp. 2565-2589 ◽  
Author(s):  
K. Meusburger ◽  
L. Mabit ◽  
J.-H. Park ◽  
T. Sandor ◽  
C. Alewell

Abstract. The aim of this study is to assess and to validate the suitability of the stable nitrogen and carbon isotope signature as soil erosion indicators in a mountain forest site in South Korea. Our approach is based on the comparison of the isotope signature of "stable" landscape positions (reference sites), which are neither affected by erosion nor deposition, with eroding sites. For undisturbed soils we expect that the enrichment of δ15N and δ13C with soil depth, due to fractionation during decomposition, goes in parallel with a decrease in nitrogen and carbon content. Soil erosion processes potentially weaken this correlation. 137Cs-method and the Revised Universal Soil Loss Equation are applied for the soil erosion quantification. The erosion rates obtained with the 137Cs method range from 0.9 t ha−1 yr−1 to 7 t ha−1 yr−1. Considering the steep slopes of up to 40° and the erosive monsoon events (R-factor of 6600 MJ mm ha−1 h−1 yr−1), the rates are plausible and within the magnitude of the RUSLE- modelled soil erosion rates, varying from 0.02 t ha−1 yr−1 to 5.1 t ha−1 yr−1. The soil profiles of the reference sites showed significant (p < 0.0001) correlations between nitrogen and carbon content and its corresponding δ15N and δ13C signatures. In contrast, for the eroding sites this relationship was weaker and for the carbon not significant. These results verify the usefulness of the stable carbon isotope signature as qualitative indicator for soil disturbance. We could show further that the δ15N isotope signature can be used similarly for uncultivated sites. We thus propose that the stable δ15N and δ13C signature of soil profiles could serve as a tool confirming the accurate choice of the reference site in soil erosion studies using the 137Cs-method.


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