试验研究了常温下活化剂对黑土磷形态及有效性的影响,结果显示:无外在磷源时,有效磷、Ca8-P和Al-P含量均随培养时间延长而增大,Ca2-P和Fe—P则减小;单施磷情况下,有效磷和Ca2-P含量随培养时间延长而减小,Ca8-P、Al—P和Fe—P增大;活化剂能促进各形态无机磷之间的转化,具有很好的增强土壤磷有效性的能力,活化能力依次为柠檬酸〉腐植酸〉活化剂H2,分别提高土壤Olsen—P含量40.93%、33.06%和23.20%。通过相关分析和回归分析得出,黑土中磷的主要组分是Ca2-P和Al-P,并得出了它们与Olsen—P的回归方程:Y(Olsen—P)-13.322+0.578X,(Ca2-P)+0.408X,(Al-P)。以期为人们研究黑土磷提供参考,为今后合理施磷提供依据。
Effects of phosphorus activator (PA) on different type of phosphorus and their validities in black soil were studied. The results showed that: Without fertilizing phosphates, the amount of Olsen-P, Cas-P and A1-P would increase along with the raise time, while Ca2-P and Fe-P were just opposite. Fertilizing phosphates, except for Cas-P, A1-P and Fe-P, they would decrease. PA which could promote inorganic P from one to another was good at increasing the concentration of Olsen-P in black soil. Three kinds of PA, with the order being citrate 〉 HA 〉H2, enhanced the concentration of Olsen-P to reach 40.93%, 33.06% and 23.20% separately. Related coefficient analysis and regression coefficient analysis were used to discuss the relation between every form inorganic phosphates and available phosphates. Available phosphates with Olsen's method mainly were Ca2-P and A1-P, their relativity with Olsen-P was obvious.The equation was established between Olsen-P and another factors that effected mainly on Olsen-P: Y = - 13.322 + 0.578Xi(Ca2-P) + 0.408X3(A1-P).