scholarly journals Observing the influences of climatic and environmental variability over soil salinity changes in the Noakhali Coastal Regions of Bangladesh using geospatial and statistical techniques

2021 ◽  
pp. 100429
Author(s):  
Umme Kawser ◽  
Biswajit Nath ◽  
Abdul Hoque
2021 ◽  
Vol 30 (1) ◽  
pp. 148-158
Author(s):  
Haneen Adeeb ◽  
Yaseen Al-Timimi

Soil salinity is one of the most important problems of land degradation, that threatening the environmental, economic and social system. The aim of this study to detect the changes in soil salinity and vegetation cover for Diyala Governorate over the period from 2005 to 2020, through the use of remote sensing techniques and geographic information system. The normalized difference vegetation index (NDVI) and salinity index (SI) were used, which were applied to four of the Landsat ETM+ and Landsat OLI satellite imagery. The results showed an increase in soil salinity from 7.27% in the period 2005–2010 to 27.03% in 2015–2020, as well as an increase in vegetation from 10% to 24% in the same period. Also the strong inverse correlation between the NDVI and the SI showed that vegetation is significantly affected and directly influenced by soil salinity changes


2012 ◽  
Vol 109 ◽  
pp. 1-10 ◽  
Author(s):  
I. Adam ◽  
D. Michot ◽  
Y. Guero ◽  
B. Soubega ◽  
I. Moussa ◽  
...  

Geoderma ◽  
2005 ◽  
Vol 125 (3-4) ◽  
pp. 287-308 ◽  
Author(s):  
J. Herrero ◽  
O. Pérez-Coveta

CATENA ◽  
2020 ◽  
Vol 195 ◽  
pp. 104912 ◽  
Author(s):  
Yongxiang Yu ◽  
Xing Li ◽  
Chengyi Zhao ◽  
Ningguo Zheng ◽  
Hongtao Jia ◽  
...  

Pedosphere ◽  
2011 ◽  
Vol 21 (4) ◽  
pp. 539-548 ◽  
Author(s):  
Chao-Yin DOU ◽  
Yao-Hu KANG ◽  
Shu-Qin WAN ◽  
Wei HU

1956 ◽  
Vol 7 (1) ◽  
pp. 20 ◽  
Author(s):  
EA Jackson ◽  
G Blackburn ◽  
ARP Clarke

Measurements have been made of seasonal changes in soil salinity and soil water at Tintinara in the Coonalpyn Downs of South Australia. Five separate sites representing different soil profiles were selected for study. All soils contained saline water-tables and four of the five had varying depths of sand over finer-textured subsoils; the fifth soil was fine-textured throughout. The investigations were conducted over a 12-month period, salinity and water determinations being made every 8 weeks. Data on soil salinity are presented as: (1) Conductance of soil pastes, determined on replicates and statistically analysed. (2) Percentage of total soluble salts, derived from conductivities of 1:5 soil-water suspensions determined on composite sample. (3) Percentage of chlorides expressed as NaCl, determined on composite samples. All sets of data show that soluble salts moved upwards through the soil profile during spring and summer and down during the rainy season. Where the summer water-table was within 4 ft of the surface large amounts of saline material accumulated in the top inch of soil; in one case there was an increase of from 0.019 per cent. NaCl in winter to 3.2 per cent. in summer. Data are also presented showing that the salinity of the ground-waters increased to a maximum of 2-3.5 per cent. total salts in spring or summer. Seasonal soil water changes are recorded and discussed in relation to salinity changes. The climatic, soil, and ground-water factors influencing salt movements are discussed and the agronomic implications of seasonal salinity changes are stressed. Suggestions on the basis of the results obtained are made respecting the sampling of saline soils.


Soil Science ◽  
1967 ◽  
Vol 104 (1) ◽  
pp. 63-68 ◽  
Author(s):  
L. C. BENZ ◽  
F. M. SANDOVAL ◽  
W. O. WILLIS

2021 ◽  
Vol 193 (5) ◽  
Author(s):  
Sophie Thiam ◽  
Grace B. Villamor ◽  
Laurice C. Faye ◽  
Jean Henri Bienvenue Sène ◽  
Badabate Diwediga ◽  
...  

AbstractSoil salinity is a major issue causing land degradation in coastal areas. In this study, we assessed the land use and soil salinity changes in Djilor district (Senegal) using remote sensing and field data. We performed land use land cover changes for the years 1984, 1994, 2007, and 2017. Electrical conductivity was measured from 300 soil samples collected at the study area; this, together with elevation, distance to river, Normalized Difference Vegetation Index (NDVI), Salinity Index (SI), and Soil-Adjusted Vegetation Index (SAVI), was used to build the salinity model using a multiple regression analysis. Supervised classification and intensity analysis were applied to determine the annual change area and the variation of gains and losses. The results showed that croplands recorded the highest gain (17%) throughout the period 1984–2017, while forest recorded 3%. The fastest annual area of change occurred during the period 1984–1994. The salinity model showed a high potential for mapping saline areas (R2 = 0.73 and RMSE = 0.68). Regarding salinity change, the slightly saline areas (2 < EC < 4 dS/m) increased by 42% whereas highly saline (EC > 8 dS/m) and moderately saline (4 < EC < 8 dS/m) areas decreased by 23% and 26%, respectively, in 2017. Additionally, the increasing salt content is less dominant in vegetated areas compared with non-vegetated areas. Nonetheless, the highly concentrated salty areas can be restored using salt-resistant plants (e.g., Eucalyptus sp., Tamarix sp.). This study gives more insights on land use planning and salinity management for improving farmers’ resilience in coastal regions.


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