Controlling soil water content in fertiliser dissolution experiments

• Published in: Nutrient cycling in agroecosystems 1999-09, Vol.55 (1), p.7-14
• Main Authors: Barlow, K. (Agriculture Victoria Ellinbank, Warragul, Vic. (Australia).), Halliwell, D, Nash, D
• Format: Article
• Language: English
• Subjects: ABONOS; Agricultural land; Agricultural management; Agricultural runoff; Agrochemicals; AGUA DEL SUELO; Algal blooms; CONTENIDO DE AGUA EN EL SUELO; EAU DU SOL; ENGRAIS; Environmental conditions; Eutrophication; Fertilizer application; FERTILIZERS; Formulations; FOSFORO; HUMEDAD RELATIVA; HUMIDITE RELATIVE; Humidity; Moisture content; PHOSPHORE; PHOSPHORUS; Potassium chloride; Rainfall; RELATIVE HUMIDITY; Resorcinol; Runoff; Saline solutions; Salt baths; Soil layers; Soil temperature; SOIL WATER; SOIL WATER CONTENT; Surface water; TENEUR EN EAU DU SOL; Water content
• ISSN: 1385-1314; 1573-0867
• DOI: 10.1023/A:1009816716466

Phosphorus lost in runoff from agricultural land leads to the enrichment of surface waters and contributes to algal blooms. Fertilisers are one source of this P. To compare the water available P of different fertiliser formulations in the laboratory it is necessary to control environmental conditions, temperature, relative humidity and soil water content, prior to simulating rainfall. Two chambers were designed in which relative humidity and soil water content were controlled using salt solutions. An initial design comprising a sealed chamber with three layers of soil samples over a salt bath was found to be inferior to a single layer design. The changes in water content of soil samples were used to test the single layer chamber in a constant temperature environment (15 °C) using a saturated KCl solution (90% relative humidity). Based on the final soil water content of the samples, the spatial variation within the chamber was within tolerable limits. The single layer chamber was used for a simulation experiment comparing the water available P of two commercial fertilisers. Using a saturated resorcinol solution (95% relative humidity) soil samples were equilibrated at 15 °C for 21 days, fertiliser added, and the water available P measured up to 600 h after fertiliser application. The results indicate that the amount of water available P was related to the fertiliser compound and exponentially related to the time since fertiliser application. It was concluded that the single layer chamber is suitable for controlling relative humidity and soil water content in trials such as these where the water available P of fertilisers are being compared.