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首页> 外文期刊>Compost Science & Utilization >Influence of Long-Term (9 yr) Composted and Stockpiled Feedlot Manure Application on Selected Soil Physical Properties of a Clay Loam Soil in Southern Alberta
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Influence of Long-Term (9 yr) Composted and Stockpiled Feedlot Manure Application on Selected Soil Physical Properties of a Clay Loam Soil in Southern Alberta

机译:长期(9年)堆肥和堆肥肥育肥施用对艾伯塔省南部粘土壤土某些土壤物理特性的影响

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Land application of composted feedlot cattle (Bos taurus) manure may have differential effects on soil physical properties compared to stockpiled manure because of the differences in the composition, particle size, and decomposability of these materials. Our objective was to determine the effect of long-term (9 yr) composted (CM) versus stockpiled (SM) manure application on selected soil physical properties. Intact soil cores were taken from CM, SM, and unamended control treatments from a long-term field experiment in the fall of 2007. Soil bulk density, plant available water (PAW), and soil water retention and hydraulic conductivity at low (0-34 kPa) water potentials were determined on the soil cores. Water retention at the 0 to 10 cm depth was significantly (P <= 0.05) greater for SM than CM between -5 and -34 kPa, suggesting an increase in transmission and storage pores in the SM treatment. In contrast, water retention at the 10 to 20 cm depth was greater for CM than SM at -1 and -5 kPa, indicating an increase in transmission pores for this treatment. Based on the results of our study, application of CM instead of SM will likely not improve most soil physical properties measured, with the exception of water retention at certain water potentials in the top two depths. However, organic amendments will likely improve most soil properties measured compared to unamended soils.
机译:与堆肥相比,堆肥育肥牛(Bos taurus)粪肥在土地上的应用对土壤物理特性可能有不同的影响,因为这些物质的成分,粒径和可分解性不同。我们的目标是确定长期(9年)堆肥(CM)与堆肥(SM)施肥对选定土壤物理特性的影响。完整的土壤核心取材自CM,SM,以及未经修正的对照处理(来自2007年秋季的长期野外试验)。土壤容重,植物有效水(PAW)以及低(0-在土壤核心上确定了34 kPa)的水势。在-5至-34 kPa之间,SM的0至10 cm深度处的保水量显着(P <= 0.05)大于CM,这表明SM处理中的传输和储存孔增加。相反,在-1和-5 kPa时,CM在10至20 cm深度处的保水量比SM更大,表明该处理的透过孔增加。根据我们的研究结果,使用CM代替SM可能不会改善大多数测得的土壤物理性质,除了在顶部两个深度处在某些水势下的保水能力。但是,与未改良的土壤相比,有机改良剂可能会改善大多数土壤特性。

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