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Titlebook: Research Developments in Saline Agriculture; Jagdish Chander Dagar,Rajender Kumar Yadav,Parbodh Book 2019 Springer Nature Singapore Pte Lt

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Modern Technologies for Diagnosis and Prognosis of Salt-affected Soils and Poor-quality Watersted soils (SAS) is distributed in 15 states and 13 agroclimatic regions. Salt deposition at low topographic zones, high evaporation in arid zone, salty parent materials and brackish ground use in peninsular plain, and inundation of saline seawater in coastal areas are primary processes controlling g
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Salinity Tolerance Indicators of soil salinity. The visual characters serve as diagnostic criteria in identifying the salt-affected soils. The physical indicators of salt-affected soils include flocculation, dispersion of clays and surface salt crusts; and conventional chemical indicators of soil salinity include electrical con
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Current Understanding of the Mangrove Forests of Indiahe sustainability of Indian mangroves are discussed. In India, mangroves are found on the east and west coasts of the mainland and on the Islands of Andaman and Nicobar and Lakshadweep. Indian mangroves represent 3.3% of global mangroves and about 56% of global mangrove species. Despite considerable
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Causes and Management of Root-zone Salinity and Sodicity in the Arid West Texas: Field-scale Experiere. This chapter focuses on causes and management of root-zone salinity and sodicity at the field scale. Available data suggest that salinity and sodicity in many agricultural fields in the region exceed the threshold levels for dominant crops (pima cotton, pecan, and alfalfa) with maximum values re
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Characterization and Problems of Saline/Sodic Vertisols and Their Management Options a prime threat to land resources, resulting in large economic and associated social consequences. The relative significance of soluble salts depends on natural drainage conditions, soil properties, groundwater quality, irrigation water quality, and management practices. Saline–sodic Vertisols and t
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Carbon Dynamics in Salt-affected Soilsde (CO.) concentrations are strongly affected by soil organic carbon (SOC) turnover. Salt affects soil C pools and CO. emission by (i) plant growth as well as C input reduction and (ii) reducing microbial activity and thus C turnover due to osmotic stress in saline soils or poor soil structure in so
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