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Relationship between cation accumulation and water content of salt‐tolerant grasses and a sedge
Author(s) -
GLENN E. P.
Publication year - 1987
Publication title -
plant, cell and environment
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.646
H-Index - 200
eISSN - 1365-3040
pISSN - 0140-7791
DOI - 10.1111/1365-3040.ep11602236
Subject(s) - halophyte , elymus , phragmites , salinity , panicum , botany , biology , poaceae , agronomy , chemistry , zoology , ecology , wetland
Salt‐tolerant grasses and a sedge were grown at three salinities in a controlled‐environment greenhouse. They were measured for growth rate, ash content, water content and cations. Fourteen species from the genera Sporobolus, Aeluropus, Leptochloa, Paspalum, Puccinellia, Hordeum, Elymus, Distichlis and Spartina survived up to the highest salt treatment (540 mol m −3 NaCl). These were designated halophytes. Eleven species from the genera Triticum, Phragmites, Dactylotenium, Cynodon, Polypogon, Panicum, Jovea and Heleocharis only survived up to 180 mol m −3 NaCl and were designated salt‐tolerant glycophytes. All species except Distichlis palmeri grew fastest on the non‐saline control treatment. All species tended to have higher Na + contents and lower K + and water contents on saline treatments compared to control plants. Halophytes differed from glycophytes in having statistically significant lower water contents on the non‐saline treatment, and lower ash contents and Na:K ratios on 180 mol m −3 . However, the range of values among species was greater than the differences between halophytes and glycophytes. All species appeared to use Na + accumulation and loss of water as the main means of osmotic adjustment. Three halophytic species were grown for a longer period of time to check the above results. The osmolality of the cell sap was measured directly by the vapour pressure method and compared to calculated values based on Na + , K + and water contents (and assuming a balancing anion such as Cl − ). Na + and K + alone could account for greater than 75% of the osmotic potential at all salinities. Hence, the accumulation of organic solutes did not appear to be an important factor in the osmotic adjustment of these species. The results support the conclusion that grasses coordinate Na + uptake and water loss to maintain a constant osmotic potential gradient between the shoot tissues and the external solution. The results were compared to a previous study with dicotyledonous halophytes at the same location.