Soil Salinity Changes Under Cropping with Lycium barbarum L. and Irrigation with Saline-Sodic Water

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

Agriculture ◽  
2021 ◽  
Vol 11 (10) ◽  
pp. 983
Author(s):  
Aadhityaa Mohanavelu ◽  
Sujay Raghavendra Naganna ◽  
Nadhir Al-Ansari

Salinity and sodicity have been a major environmental hazard of the past century since more than 25% of the total land and 33% of the irrigated land globally are affected by salinity and sodicity. Adverse effects of soil salinity and sodicity include inhibited crop growth, waterlogging issues, groundwater contamination, loss in soil fertility and other associated secondary impacts on dependent ecosystems. Salinity and sodicity also have an enormous impact on food security since a substantial portion of the world’s irrigated land is affected by them. While the intrinsic nature of the soil could cause soil salinity and sodicity, in developing countries, they are also primarily caused by unsustainable irrigation practices, such as using high volumes of fertilizers, irrigating with saline/sodic water and lack of adequate drainage facilities to drain surplus irrigated water. This has also caused irreversible groundwater contamination in many regions. Although several remediation techniques have been developed, comprehensive land reclamation still remains challenging and is often time and resource inefficient. Mitigating the risk of salinity and sodicity while continuing to irrigate the land, for example, by growing salt-resistant crops such as halophytes together with regular crops or creating artificial drainage appears to be the most practical solution as farmers cannot halt irrigation. The purpose of this review is to highlight the global prevalence of salinity and sodicity in irrigated areas, highlight their spatiotemporal variability and causes, document the effects of irrigation induced salinity and sodicity on physicochemical properties of soil and groundwater, and discuss practical, innovative, and feasible practices and solutions to mitigate the salinity and sodicity hazards on soil and groundwater.


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

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