Arid Soil Research and Rehabilitation · 1992 · 42 citations · 11 references
AgricultureAgronomySoil SciencesPlant NutritionSoil SalinitySoil SciencePhosphorus CyclePhosphorus ManagementPhosphorus NutritionSalinity Effects On Soil PropertiesSalinity Stress PhysiologySoil Phosphorus ChemistryCrop YieldsGreenhouse TrialsPhosphate Availability In SoilPhosphorus RequirementSalinity ToleranceSoil Fertility Under SalinitySoil Phosphorus AvailabilitySoil Solution Salinity
Abstract In a greenhouse study, table pea (Pisum sativum L.) was grown from sowing to maturity in Cl‐‐dominated (Cl‐ : SC2‐ 4 = 7:3) and SO2‐ 4‐dominated (Cl‐ : SO2‐ 4 =3:7) saline sandy soil (Typic Torripsamments) at comparable electrical conductivities (ECe 4, 6, and 8 dS m‐1). Each salinity treatment, including the nonsaline control, contained four levels of added P (0, 20, 40, and 80 mg P kg‐1 soil). In P control (Olsen's P 3.5 mg kg‐1), grain yields at ECe 4, 6, and 8 dS m‐1 were 58, 17, and 7% in Cl‐‐dominated salinity and 91, 48, and 37%, respectively, in SO2‐ 4‐dominated salinity. At 20 mg P kg‐1 level (Olsen's P 13 mg kg‐1), grain yields for the respective ECe values were 108, 49, and 13 % in Cl‐‐dominated salinity and 138, 106, and 75% in SO2‐ 4‐dominated salinity, whereas at 80 mg P kg‐1 level (Olsen's P 46 mg kg‐1) yields were 140, 80, and 17% in Cl‐‐dominated salinity and 100, 108, and 128% in SO2‐ 4‐dominated salinity relative to the nonsaline soil. The P requirement at ECe 6 dS m‐1 was twice that of the nonsaline soil in Cl‐‐dominated and equal to that of the nonsaline soil in the SO2‐ 4‐dominated salinity. However, at ECe 8 dS m‐1, the indicator crop did not respond to P level in Cl‐ ‐dominated salinity, while in SO2‐ 4 ‐dominated salinity, its requirement for P was twice that of the nonsaline soil. As the response to applications of P decreased with the increase in Cl content of soil, it appeared that P enhancement of salinity tolerance depended on a certain threshold value of Cl content in the root zone, which was 50 mmol L‐1 for table pea. The deleterious effect of Cl‐ ‐dominated salinity at ECe 8 dS m‐1 (Cl‐ = 73.5 mmol L‐1), irrespective of the P content of soil, appeared to be due to excessive accumulation of Cl (over 6%) and a sharp reduction (54–78%) in the S content of straw, possibly due to the impedence in the translocation of S by Cl at the root‐shoot interphase. Plants grown in Cl‐‐dominated salinity also had considerably less K, Mg, and Na, but more Ca and N in their straw than those grown in SO2‐ 4 ‐dominated salinity.
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