Pot experiment was conducted to examine how application of KH2PO4 （0-165 mg·kg^-1 P） to affect nutrient ion uptake and rhizosphere acidification of soybean （Glycine max L.） grown in greenhouse for 90 days. Wh...Pot experiment was conducted to examine how application of KH2PO4 （0-165 mg·kg^-1 P） to affect nutrient ion uptake and rhizosphere acidification of soybean （Glycine max L.） grown in greenhouse for 90 days. When supplied of 82 and 165 mg·kg^-1 P, soybeans showed excessive poison. Under all kinds of P levels, the K, Ca, Na and Mg concents in plant tissues were as below order K was nodules 〉 roots 〉 pods 〉 shoots; Ca was shoots 〉 roots 〉 nodules 〉 pods; Na was roots 〉 nodules 〉 pods 〉 shoots and Mg was shoots 〉 nodules 〉 roots 〉 pods. K concent in plant tisssues had greater effect on rhizosphere acidification than other cations in this experiment irrespective of P supply, and was significantly negative to pH. Na concentration was significantly positive to pH. Excessive P supply induced rhizosphere acidification, pH decreased as P supply increased from 82 to 165 mg·kg^-1. Ash alkalinity in shoots and roots was significantly positively correlated with rhizosphere pH irrespective of P supply. All these results suggested that P supply affected nutrient uptake, induced ash alkalinity to increase and rhizosphere pH to decrease in soybean.展开更多
基金Supported by Innovative Research Team of Northeast Agricultural University
文摘Pot experiment was conducted to examine how application of KH2PO4 （0-165 mg·kg^-1 P） to affect nutrient ion uptake and rhizosphere acidification of soybean （Glycine max L.） grown in greenhouse for 90 days. When supplied of 82 and 165 mg·kg^-1 P, soybeans showed excessive poison. Under all kinds of P levels, the K, Ca, Na and Mg concents in plant tissues were as below order K was nodules 〉 roots 〉 pods 〉 shoots; Ca was shoots 〉 roots 〉 nodules 〉 pods; Na was roots 〉 nodules 〉 pods 〉 shoots and Mg was shoots 〉 nodules 〉 roots 〉 pods. K concent in plant tisssues had greater effect on rhizosphere acidification than other cations in this experiment irrespective of P supply, and was significantly negative to pH. Na concentration was significantly positive to pH. Excessive P supply induced rhizosphere acidification, pH decreased as P supply increased from 82 to 165 mg·kg^-1. Ash alkalinity in shoots and roots was significantly positively correlated with rhizosphere pH irrespective of P supply. All these results suggested that P supply affected nutrient uptake, induced ash alkalinity to increase and rhizosphere pH to decrease in soybean.
