POTASSIUM BALANCE AND RELEASE KINETICS UNDER RICE-RICE CROPPING SYSTEM Dr. A.K. Pal, Professor Dr. A.K. Dash, Assoc. Professor Department of Soil Science and Agricultural Chemistry College of Agriculture, OUAT, Bhubaneswar-3 Different forms of K in increasing order of availability Mineral / structural K (Unavailable ) Non exchangeable/fixed K ( difficultly available/ slowly available) Exchangeable K (Easily available) Water soluble K (Readily available) Exch. K (on external surface) Rapid and continuous exchange Slow and Contigent exchange K in solution Fixed or reverted K K definitely fixed (Barbier, 1962) Factors affecting availability of K in soils of Orissa Effect of particle size and distribution Effect of mineralogy and weathering Effect of soil reaction Effect of soil moisture regime Effect of previous cropping and management Effect of CEC and associated cations Contribution from subsoil Different forms of K in Orissa Soil Broad Soil Group Total K2O% Non Exch. Fixed K (me/100g) Exch. K (me/100 g) KSaturated (%) Water soluble K (me/L) Textural class Laterite Soils 0.3-1.2 (0.69) 0.10-0.91 (0.31) 0.06-0.30 (0.17) 1.30-4.80 (2.7) 0.008-0.08 (0.05) Sandy loam to silty loam Red soil, mixed red & black soil 1.62-6.03 (3.2) 0.20-0.97 (0.68) 0.10-1.10 (0.40) 0.75-14.90 (5.54) 0.025-0.27 (0.14) Loam to clay Alluvial soils 0.68-2.41 (1.32) 0.05-1.92 (0.85) 0.06-0.64 (0.26) 0.81-5.80 (2.35) 0.018-0.175 (0.07) Sandy loam to clay Coastal saline soils 1.77-3.01 2.49 0.18-1.45 (0.72) 0.14-1.60 (0.89) 3.0-6.19 (4.32) 0.30-1.60 (0.73) Loam to clay Figures in parenthesis indicate average value Mean annual yield, K-uptake, K balance in the soil after 20 years of rice cropping Treatments 100%N 100% NP 100% NPK 100% NPK+FYM 150% NPK N0P0K0 (Control) Mean yield of rice(q/ha) Mean annual K-uptake (kg/ha) Annual K-balance (kg/ha) Kharif Rabi 20.95 22.52 29.82 34.81 20.50 27.98 32.10 37.59 84.00 90.00 137.00 167.00 -84.00 -90.00 -37.00 -47.00 30.13 15.60 34.00 13.99 157.00 56.00 -7.00 -56.00 Cumulative effect of treatments on NH4OAc extractable –K over 20 years of rice-rice cropping Tr. No Treatments NH4OAc(mg/kg soil) 0-15 cm layer 15-30 cm layer 30-45 cm layer Total 1 150 % NPK 23 26 40 89 2 100% NPK 20 21 34 75 3 100% NPK+ Zn 20 20 36 76 4 100% NP 17 18 28 63 5 100% N 17 17 28 62 6 100% NPK +FYM 28 25 41 94 7 100% NPK(- S) 22 22 34 78 8 Lime+ NPK (STB) 26 29 39 94 9 Control Initial 14 13 21 48 12.5 22 35.5 70 Cumulative effect of treatments on 1N HNO3 boiling(one time) extractable–K over 20 years of cropping Tr. Treatment No 1N HNO3 (mg/kg soil) 0-15 cm layer 15-30 cm layer 30-45 cm layer Total 1 150 % NPK 125 125 133 430 2 100% NPK 107 96 138 351 3 100% NPK+ Zn 107 107 180 355 4 100% NP 73 85 148 279 5 100% N 83 93 141 304 6 100% NPK +FYM 99 87 121 305 7 100% NPK(- S) 100 101 128 340 8 Lime+ NPK (STB) 128 108 119 395 9 Control 77 88 139 288 120 116.5 156.5 393 Initial Cumulative effect of treatments on Non exchangable–K over 20 years of cropping (1N HNO3 - NH4OAc) (mg/kg soil) Tr. No Treatment 0-15 cm layer 15-30 cm layer 30-45 cm layer Total 1 150 % NPK 102 99 140 341 2 100% NPK 87 75 114 276 3 100% NPK+ Zn 87 87 105 279 4 100% NP 56 67 93 216 5 100% N 66 76 100 242 6 100% NPK +FYM 71 62 108 241 7 100% NPK(- S) 78 79 105 262 8 Lime+ NPK (STB) 102 79 120 301 107.5 94.5 121 323 Initial Cumulative Effect of Treatments on Step-K and constant rate-k after 40 cropping cycles Tr. No. CR-K (mg kg-1) Step K (mg kg-1) Treatment 1 3 4 6 8 50 % NPK 150 % NPK 100 % NPK 100 % NP 100 % NPK +FYM 10 Lime + (soil test based) Initial 0-15 cm layer 15-30 cm layer 30-45 cm layer 0-15 cm layer 15-30 cm layer 30-45 cm layer 71 98 84 43 72 79 88 84 51 54 85 105 108 74 97 16 17 16 15 16 18 18 18 16 17 23 25 24 22 24 96 96 74 97 108 111 17 17 19 20 25 26 Mean annual K application, K - uptake and K balance (kg ha-1) of different treatments (14 cropping cycle) Treatments Mean annual application of K 100% NPK + Zn + B + 100 S 100% NPK + Zn + B 100 100% NPK + B + S 100 100% NPK + Zn + S 100 100% NPK + Zn + B + 100 S + FYM 100% NPK + Zn + B + 100 S + GM 100% NK + Zn + B + 155.6 S + Straw Control - Mean annual K-uptake Mean annual balance 121.2 -21.2 118.0 118.1 113.6 118.0 -18.0 -18.1 -13.6 -18.0 109.4 -9.4 109.8 45.8 61.7 -61.7 PHYSICO- CHEMICAL PROPERTIES OF SOILS Block No. of samples pH OC (%) CEC cmol (p+) kg-1) Clay (%) Narasinghpur 21 5.14-8.1 0.44-1.40 8.71-22.39 10.7-34.1 Baramba 22 4.96-8.3 0.51-1.14 14.74-44.44 12.4-43.8 Athagarh 22 4.66-5.97 0.33-1.38 9.89-35.44 90.0-41.0 Tigiria 20 5.09-7.44 0.33-1.22 9.09-39.39 10.4-35.0 MEAN VALUE OF DIFFERENT FORMS OF POTASSIUM Forms of K (mg kg-1 soil) Block NH4 OAc Non extractable exchangeable Lattice Total Narasinghpur 10-380 130-900 750-1620 950-3000 Baramba 22-125 230-925 220-1570 60-2050 Athagarh 45-170 155-845 380-1850 900-2900 Tigiria 45-125 145-740 700-2360 1000-2900 Correlation coefficient among different forms of K Form of potassium Water soluble K Exchangeable- K Available K NonExch. K Lattic K Total K Water soluble K 1.000 Exchangeable K 0.714** 1.000 Available K 0.812** 0.989** 1.000 Non – Exch. K 0.53/** 0.365 0.421 1.000 Lattice K 0.381 0.200 0.279 0.381 Total K 0.517* 0.322 0.300 0.671** 0.940** 1.000 * Significant at P = 0.05, ** - Significant at P = 0.01 1.000 Release of K extracted by boiling with 1N HNO3 1st 2nd 3rd K released (mg kg-1 soil) 4th 5th 6th 7th 8th 9th 10th 150 325 375 200 250 175 675 150 175 150 175 375 225 175 475 275 425 400 275 700 325 50 175 325 100 150 150 525 100 95 75 120 150 150 64 350 175 325 325 175 450 96 44 74 106 8 64 75 122 75 80 56 76 54 75 54 104 58 104 112 72 188 70 40 54 96 40 50 52 80 60 64 46 52 36 56 48 84 42 70 92 56 136 56 36 28 46 28 26 44 28 46 40 34 20 24 26 42 38 12 28 46 36 56 48 36 28 46 28 26 44 28 46 40 34 20 24 26 42 38 12 28 46 36 56 48 36 28 46 28 26 44 28 46 40 34 20 24 26 42 38 12 28 46 36 56 48 Sample No. N1 N2 N3 N4 N5 N6 N7 N8 N9 N10 N11 N12 N13 N14 N15 N16 N17 N18 N19 N20 N21 36 36 62 30 44 46 40 56 60 40 38 24 42 44 66 30 50 70 48 104 50 36 28 52 28 28 44 30 50 56 34 28 24 36 42 48 16 38 58 40 90 48 36 28 46 28 26 44 28 46 40 34 20 24 26 42 38 12 28 46 36 56 48 CR-K Total step K 36 28 46 28 26 44 28 46 40 34 20 24 26 42 38 12 28 46 36 56 48 140 524 740 288 430 278 1312 215 290 197 369 519 428 283 899 524 844 781 450 1332 709 Total extract able K 500 804 1200 568 690 718 1592 675 690 537 869 759 688 703 1279 644 1124 1241 810 1892 1189 Correlation coefficient of K release parameter with forms of K NH4OAC-K NonExch. K Lattice K Total K NHOAC-K 1.000 Non exch-K 0.821** 1.000 Lattic K 0.448* 0.418 Total K 0.689** 0.733** 0.921** 1.000 CR-K 0.510* 0.249 Total Steb K 0.736** Total 0.810** Extractable K CR-K Total step K Total extractable K 1.000 0.478* 0.489* 1.000 0.969** 0.399 0.710** 0.206 1.000 0.944** 0.498* 0.781** 0.676 0.959** 1.000 Changes in the values of K release parameters with depth in the profiles Genetic horizon Depth (cm) Total extract. K Total step K CR – K % of non-exch. K + Lattice K Mg kg-1 Ap B 21t B 22t B 23t C 0-11 11-52 52-88 88-115 115-150 Ap B 21t B 22t B 23t 0-14 14-42 42-90 90-172 Ap B 21t B 22t B 23t 0-14 14-27 27-60 60-150 Ap B 21t B 22t C 0-14 14-32 32-84 84-155 Total extract K Profile – 2 Upper ridge (Aridic Kanhapulstlfs) 1365 1325 04 54.9 2008 1768 24 74.9 2228 1908 32 76.8 2466 2066 40 88.4 2505 2105 40 96.9 Profile – 3 Mid upland (Aridic Kanhaplustalfs) 1348 1188 16 63.6 2085 18545 24 77.1 2776 2216 56 95.7 2882 2282 60 85.0 Profile – 4 Medium land (Aridic Kanhaplustalfs) 1432 1352 08 83.4 1629 1389 24 76.7 2106 1786 32 87.4 2709 2069 64 86.7 Profile – 5 Medium valley alnd (Aridic Ustochrepts) 1109 909 20 82.5 1390 1070 32 97.2 1787 1587 20 63.9 2185 1865 32 73.2 Total Step K CR-K 53.3 66.6 65.8 74.1 81.4 0.2 0.9 1.1 1.4 1.5 56.0 68.2 76.4 67.3 0.8 0.9 0.9 0.8 78.8 65.4 74.1 66.2 0.5 1.1 1.3 2.0 67.6 74.8 56.8 62.5 1.5 2.2 0.7 1.1 Relationship of the K-release with forms of K (n = 17) K – release parameters Clay NonLattice Total K exchangea K ble K Total extractable K 0.96** 0.73** 0.84** 0.95** Total step K 0.95** 0.79** 0.89** 0.94** CR-K 0.80** NS 0.58* 0.81** CONCLUSION Potassium dose should be increased to sustain the crop productivity as well as soil health. Straw recycling should be advocated for better management of K deficiency in rice-rice cropping system. Dynamic equilibrium among different forms of K is maintained in soil. Higher amount of step K indicates more release of K from non-exchangeable form under stress condition. Higher value of extractable K in soil indicates greater Ksupplying capacity. Higher value of CR-K indicates adequately supply of K to the plant. Step K is highly correlated with clay content of soil. K-release characteristics revealed that IN HNO3 can serve as a good index of K availability from nonexchangeable and lattice K.
© Copyright 2026 Paperzz