白浆土－植物系统营养物质转化机制及其有效性研究Ⅰ．~（32）P同位素示踪法对白浆土中P肥利用率

利用３２Ｐ同位素示踪法对白浆土中Ｐ肥利用率进行了研究．结果表明，在岗地白浆土上，表层土壤表现出一定程度的供Ｐ不足现象，白浆层土壤有效Ｐ含量严重缺乏．表层土壤中当季Ｐ肥利用率的变幅范围为６．０９～１２．３５％，白浆层土壤Ｐ肥利用率为１３％左右．施用有机肥能明显提高白浆土ＯｌｓｅｎＰ的含量，加速土壤本身Ｐ的活化，各种有机物中，以猪粪对土壤潜在Ｐ的活化效果最好．将ＯｌｓｅｎＰ与Ｘ值、Ａ值比较，认为ＯｌｓｅｎＰ是评价白浆上Ｐ肥力简便易行的可靠指标．

Thermochemical and thermal analysis on N-(p-methylphenyl)-N '-(2-pyridyl)urea

Low temperature heat capacities of N-(p-methylphenyl)-N'-(2-pyridyl)urea were determined by adiabatic calorimetry method in the temperature range from 80 to 370 K. It was found that there was not any heat anomaly in this temperature region. Based on the experimental data, some thermodynamic function results were obtained. Thermal stability and decomposition characteristics analysis of N-(p-methylphenyl)-N'-(2-pyridyl)urea were carried out by DSC and TG. The results indicated that N-(p-methylphenyl)-N'-(2-pyridyl)urea started to melt at ca. 426 K (153degreesC) and the melting peak located at 447.01 K (173.86degreesC). The melting enthalpy was 204.445 kJ mol(-1) (899.6 J g(-1)). The decomposition peak of N-(p-methylphenyl)-N'-(2-pyridyl)urea was found at 499.26 K (226.11degreesC) from DSC curve. This result was similar with that from TG and DTG experiment, in which the mass loss peak was determined as 500.4 K (227.2degreesC).