![]() international fertilizer correspondent No 5 |
A pot experiment was conducted to test five extractants for K extraction from six soil series in Punjab, Pakistan for their correlation with K uptake by wheat. The efficiency of the extractants was in the order of H2O < CaCl2 < MgOAc < NH4OAc < HNO3. Significant correlation was found between extracted soil K and K in grains and straw. It is suggested that 1 N NH4OAc, 0.5 N MgOAc or 0.025 N CaCl2 can be used for K indexing.
Cumin holds an important economic position in the agriculture of Baluchistan, Pakistan, but farmers in this area are not aware of the importance of fertilizers. The study was conducted to find out the most suitable combination of NPK. The highest seed yield (1180 kg/ha) was recorded with 120-60-30 kg/ha N-P2O5-K2O.
The study was conducted to determine the non-exch. K pool of the sand and silt fraction in soils in relation to their mineralogical composition. In less weathered alluvial soils the sand fraction released higher K quantities in boiling HNO3 acid. In moderately weathered soils the silt fraction became the major source of K released in boiling HNO3. Highly weathered soils released lower HNO3 extractable K from the sand and the silt fraction than other alluvial soils, which suggested that HNO3 extracted K follows the degree of profile development.
Potassium fixation in alluvial soils is influenced by the weathering stage. Moderately weathered soils were found to have the highest fixation capacity compared to highly weathered or less weathered soils. In contrast to other findings, K fixation did not relate to the clay content.
In a greenhouse study the effect of K sources, the rate of application and moisture regimes was investigated on sorghum yield and K and S uptake. Use of potassium sulphate gave higher dry matter yield and led to higher K and S uptake than potassium chloride. Soil water depletion reduces dry matter yield of sorghum and affected K and S uptake.
The effect of potash use on the soil K status was investigated in South India in a long-term experiment with a finger millet-maize-cowpea rotation. The results indicate that none of the crops responded to potash use because of the high level of initial soil K. However, over the years, total K and exchangeable K levels in soils were found to decline, irrespective of the nutrient input, i.e. whether K was added or not. The strongest soil K depletion occurred under the N and NP treatment. The observed K depletion in cases where K fertilizers were added suggests higher K uptake due to luxury consumption. The observed soil K mining would in the long run limit crop yields and render the land chemically degraded.