3 research outputs found
Downstream hydrochemistry and irrigation water quality of the Syr Darya, Aral Sea Basin, South Kazakhstan
New hydrochemical measurements from the Syr Darya provide insights into factors affecting the composition and quality of a major freshwater source replenishing the Aral Sea. This river is heavily used for power and irrigation and crosses territories of four Central Asia republics. It is intensely managed, draining several major tributaries, many reservoirs, and numerous irrigation distribution systems and canals. Analysis of seasonal changes in dissolved ion concentrations using geochemical diagrams, elemental ratios, statistical correlation, and equilibrium modeling allowed the characterization of mineral formation processes that control the dissolved chemical composition. Measured water hydrochemistry and composition type differs substantially from previous reports from the upper reaches of the Syr Darya in Kyrgyzstan. Element ratios, statistical correlation, and the presence of NO3- and NO2- suggest that the downstream trend of increasing total dissolved solids (TDS) from Zhetysay city to the Aral Sea in June is controlled by evaporationβcrystallization processes, which contribute to the river dissolved load through soil runoff and return irrigation waters following leaching of secondary salts. Downstream sample composition during the growing season shows significant changes in magnesium-to-calcium ratios in the river water. Elevated magnesium levels in Syr Darya waters may pose a problem to sustainable uses for irrigation
ΠΠΈΠ΄ΡΠΎΡΠ΅ΡΠΌΠ°Π»ΡΠ½ΡΠΉ ΡΠΈΠ½ΡΠ΅Π· ΠΌΠΎΠ½ΠΎΡΡΡΡΠΊΡΡΡΠ½ΠΎΠ³ΠΎ LaPO4: ΠΌΠΎΡΡΠΎΠ»ΠΎΠ³ΠΈΡ ΠΈ ΡΡΡΡΠΊΡΡΡΠ°
ΠΠ±Π»Π°ΡΡΡ ΠΏΡΠΈΠΌΠ΅Π½Π΅Π½ΠΈΡ ΠΌΠ°ΡΠ΅ΡΠΈΠ°Π»ΠΎΠ² Π½Π° ΠΎΡΠ½ΠΎΠ²Π΅ ΠΎΡΡΠΎΡΠΎΡΡΠ°ΡΠ° Π»Π°Π½ΡΠ°Π½Π° (LaPO4), Π² ΡΠΎΠΌ ΡΠΈΡΠ»Π΅ Π½Π°Π½ΠΎΠΌΠ°ΡΠ΅ΡΠΈΠ°Π»ΠΎΠ², Π² ΠΏΠΎΡΠ»Π΅Π΄Π½Π΅Π΅ Π²ΡΠ΅ΠΌΡ ΠΏΠΎΡΡΠΎΡΠ½Π½ΠΎ ΡΠ°ΡΡΠΈΡΡΠ΅ΡΡΡ. ΠΡΡΠΎΠΊΠΈΠΉ ΡΡΠΎΠ²Π΅Π½Ρ ΠΌΠ΅Ρ
Π°Π½ΠΈΡΠ΅ΡΠΊΠΈΡ
ΡΠ²ΠΎΠΉΡΡΠ² ΠΈ ΡΠΎΠ²ΠΌΠ΅ΡΡΠΈΠΌΠΎΡΡΡ ΡΠΎ ΠΌΠ½ΠΎΠ³ΠΈΠΌΠΈ ΠΎΠΊΡΠΈΠ΄Π°ΠΌΠΈ ΠΏΠΎΠ·Π²ΠΎΠ»ΡΡΡ ΡΠ°ΡΡΠΌΠ°ΡΡΠΈΠ²Π°ΡΡ Π²ΠΎΠ·ΠΌΠΎΠΆΠ½ΠΎΡΡΡ ΠΈΡΒΠΏΠΎΠ»ΡΠ·ΠΎΠ²Π°Π½ΠΈΡ ΠΎΡΡΠΎΡΠΎΡΡΠ°ΡΠ° Π»Π°Π½ΡΠ°Π½Π° Π² ΠΊΠ°ΡΠ΅ΡΡΠ²Π΅ ΠΊΠΎΠΌΠΏΠΎΠ½Π΅Π½ΡΠ° ΠΊΠΎΠΌΠΏΠΎΠ·ΠΈΡΠΈΠΎΠ½Π½ΠΎΠ³ΠΎ ΠΌΠ°ΡΠ΅ΡΠΈΠ°Π»Π° ΠΊΠΎΠ½ΒΡΡΡΡΠΊΡΠΈΠΎΠ½Π½ΠΎΠ³ΠΎ Π½Π°Π·Π½Π°ΡΠ΅Π½ΠΈΡ. Π’Π°ΠΊΠΎΠ΅ ΠΏΡΠΈΠΌΠ΅Π½Π΅Π½ΠΈΠ΅ ΠΎΡΠΎΠ±Π΅Π½Π½ΠΎ ΠΏΠ΅ΡΡΠΏΠ΅ΠΊΡΠΈΠ²Π½ΠΎ ΠΏΡΠΈ ΠΈΡΠΏΠΎΠ»ΡΠ·ΠΎΠ²Π°Π½ΠΈΠΈ Π½Π°Π½ΠΎΡΠ°ΡΡΠΈΡ Ρ ΠΊΠ²Π°Π·ΠΈΠΎΠ΄Π½ΠΎΠΌΠ΅ΡΠ½ΠΎΠΉ ΠΌΠΎΡΡΠΎΠ»ΠΎΠ³ΠΈΠ΅ΠΉ (Π½Π°Π½ΠΎΡΡΠ΅ΡΠΆΠ½Π΅ΠΉ). ΠΠΎΠ»ΡΡΠ°Ρ ΠΈΠ·ΠΎΠΌΠΎΡΡΠ½Π°Ρ ΡΠΌΠΊΠΎΡΡΡ ΡΠ°Π·Ρ Π½Π° ΠΎΡΠ½ΠΎΠ²Π΅ LaPO4 ΠΏΠΎ ΠΎΡΠ½ΠΎΡΠ΅Π½ΠΈΡ ΠΊ ΡΡΠ»ΠΎΡΠ½ΠΎΠ·Π΅ΠΌΠ΅Π»ΡΠ½ΡΠΌ ΠΈΠΎΠ½Π°ΠΌ, ΠΈΠΎΠ½Π°ΠΌ Π»Π°Π½ΡΠ°Π½ΠΎΠΈΠ΄ΠΎΠ² ΠΈ Π°ΠΊΡΠΈΒΠ½ΠΎΠΈΠ΄ΠΎΠ², Π²ΡΡΠΎΠΊΠ°Ρ Ρ
ΠΈΠΌΠΈΡΠ΅ΡΠΊΠ°Ρ ΠΈ ΡΠ°Π΄ΠΈΠ°ΡΠΈΠΎΠ½Π½Π°Ρ ΡΡΠΎΠΉΠΊΠΎΡΡΡ Π΄Π΅Π»Π°ΡΡ ΠΏΠ΅ΡΡΠΏΠ΅ΠΊΡΠΈΠ²Π½ΡΠΌ ΠΈΡΠΏΠΎΠ»ΡΠ·ΠΎΠ²Π°ΒΠ½ΠΈΠ΅ ΡΡΠΎΠ³ΠΎ ΡΠΎΠ΅Π΄ΠΈΠ½Π΅Π½ΠΈΡ Π² ΠΊΠ°ΡΠ΅ΡΡΠ²Π΅ ΠΌΠ°ΡΡΠΈΡΡ Π΄Π»Ρ ΠΈΠΌΠΌΠΎΠ±ΠΈΠ»ΠΈΠ·Π°ΡΠΈΠΈ ΡΠ°Π΄ΠΈΠΎΠ°ΠΊΡΠΈΠ²Π½ΡΡ
ΠΎΡΡ
ΠΎΠ΄ΠΎΠ².
Π ΡΠ°Π±ΠΎΡΠ΅ ΡΠ°ΡΡΠΌΠ°ΡΡΠΈΠ²Π°Π΅ΡΡΡ Π²ΠΎΠ·ΠΌΠΎΠΆΠ½ΠΎΡΡΡ ΠΏΠΎΠ»ΡΡΠ΅Π½ΠΈΡ ΠΎΡΡΠΎΡΠΎΡΡΠ°ΡΠ° Π»Π°Π½ΡΠ°Π½Π° (LaPO4) Π³ΠΈΠ΄ΡΠΎΒΡΠ΅ΡΠΌΠ°Π»ΡΠ½ΡΠΌ ΠΌΠ΅ΡΠΎΠ΄ΠΎΠΌ. ΠΡΠΈΠ²Π΅Π΄Π΅Π½Ρ ΡΠ΅Π·ΡΠ»ΡΡΠ°ΡΡ ΠΈΡΡΠ»Π΅Π΄ΠΎΠ²Π°Π½ΠΈΡ Π²Π»ΠΈΡΠ½ΠΈΡ ΡΠ, ΡΠ΅ΠΌΠΏΠ΅ΡΠ°ΡΡΡΡ ΠΈ Π²ΡΠ΅ΒΠΌΠ΅Π½ΠΈ ΠΎΠ±ΡΠ°Π±ΠΎΡΠΊΠΈ ΠΈ Π³ΠΈΠ΄ΡΠΎΡΠ΅ΡΠΌΠ°Π»ΡΠ½ΠΎΠ³ΠΎ ΡΠΈΠ½ΡΠ΅Π·Π° Π½Π° ΠΌΠΎΡΡΠΎΠ»ΠΎΠ³ΠΈΡ ΠΈ ΡΡΡΡΠΊΡΡΡΡ ΠΌΠΎΠ½ΠΎΡΡΡΡΠΊΡΡΡΠ½ΠΎΠ³ΠΎ ΡΠΎΡΡΠ°ΡΠ° Π»Π°Π½ΡΠ°Π½Π°. Π£ΡΡΠ°Π½ΠΎΠ²Π»Π΅Π½ΠΎ, ΡΡΠΎ Ρ ΡΠΎΡΡΠΎΠΌ ΡΠ ΠΌΠ΅Π½ΡΠ΅ΡΡΡ ΠΌΠΎΡΡΠΎΠ»ΠΎΠ³ΠΈΡ ΡΠΎΡΡΠ°ΡΠ° ΠΈ ΡΠ°Π·ΠΌΠ΅ΡΡ ΠΊΡΠΈΡΡΠ°Π»Π»ΠΈΡΠΎΠ², ΠΏΡΠΈ ΡΡΠΎΠΌ Π½Π°Π±Π»ΡΠ΄Π°Π΅ΡΡΡ ΠΏΠ΅ΡΠ΅Ρ
ΠΎΠ΄ ΠΊΡΠΈΡΡΠ°Π»Π»ΠΈΡΠ΅ΡΠΊΠΎΠΉ ΡΡΡΡΠΊΡΡΡΡ Ρ Π³Π΅ΠΊΡΠ°Π³ΠΎΠ½Π°Π»ΡΠ½ΠΎΠΉ Π² ΠΌΠΎΠ½ΠΎΠΊΠ»ΠΈΠ½Π½ΡΡ
Downstream hydrochemistry and irrigation water quality of the Syr Darya, Aral Sea Basin, South Kazakhstan
New hydrochemical measurements from the Syr Darya provide insights into factors affecting the composition and quality of a major freshwater source replenishing the Aral Sea. This river is heavily used for power and irrigation and crosses territories of four Central Asia republics. It is intensely managed, draining several major tributaries, many reservoirs, and numerous irrigation distribution systems and canals. Analysis of seasonal changes in dissolved ion concentrations using geochemical diagrams, elemental ratios, statistical correlation, and equilibrium modeling allowed the characterization of mineral formation processes that control the dissolved chemical composition. Measured water hydrochemistry and composition type differs substantially from previous reports from the upper reaches of the Syr Darya in Kyrgyzstan. Element ratios, statistical correlation, and the presence of NO3- and NO2- suggest that the downstream trend of increasing total dissolved solids (TDS) from Zhetysay city to the Aral Sea in June is controlled by evaporationβcrystallization processes, which contribute to the river dissolved load through soil runoff and return irrigation waters following leaching of secondary salts. Downstream sample composition during the growing season shows significant changes in magnesium-to-calcium ratios in the river water. Elevated magnesium levels in Syr Darya waters may pose a problem to sustainable uses for irrigation.
HIGHLIGHTS
Water composition transitions from CaβMgβHCO3 to CaβMgβSO4βCl to NaβSO4βCl downstream the Syr Darya.;
Seasonal and downstream differences in composition suggest that irrigation water inputs are likely controlled by different mineral equilibria.;
Water quality indices showed that, generally, Syr Darya water is suitable for irrigation.