首页> 外文期刊>Journal of the Minnesota Academy of Science >Relative Soil Aeration in a Cultivated Prairie Pothole
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Relative Soil Aeration in a Cultivated Prairie Pothole

机译:耕地大坑中的相对土壤通气

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Many small prairie potholes receive surface runoff from their catchments and serve as a focal point of ground water recharge. Soil aeration controls the solubility and form of many soil chemicals. Platinum electrodes are sensitive to oxygen and provide a very sensitive indicator of its presence. Electrodes were installed at the 15-, 30-, and 45-cm depth across two transects within a shallow, cultivated depression which serves as a recharge site for groundwater. Soils on the rim of the depression remained aerobic throughout two consecutive cropping years even at 45 cm. Soils within the depression became anaerobic briefly in the first year and very intensely anaerobic in the second year. Electrode potentials decreased with depth. Values of -250 mV were measured at 45 cm and these values suggest that sulfate-S was reduced to sulfide-S within the depression. Because the subsoil was anaerobic, all nitrate-N should be reduced to nitrogen gas. Thus, leaching of nitrate-N into the groundwater during the growing season is a very unlikely event. The degree of anaerobiosis was sufficient to dissolve iron and manganese oxides; organic chemicals adsorbed to these oxide surfaces may be at increased risk of leaching into groundwater.
机译:许多小草原坑洼地从其流域接收地表径流,并作为地下水补给的重点。土壤通气控制着许多土壤化学物质的溶解度和形式。铂电极对氧气很敏感,并提供了非常敏感的氧气指示。将电极安装在15厘米,30厘米和45厘米深度处,穿过一个浅的耕种洼地中的两个横断面,该洼地用作地下水的补给站。在连续两个种植年度中,凹陷边缘的土壤即使在45厘米处也保持需氧状态。凹陷内的土壤在第一年短暂变为厌氧状态,第二年变得非常厌氧。电极电位随深度降低。在45 cm处测量到-250 mV的值,这些值表明在凹陷内硫酸盐-S还原为硫化物-S。由于底土是厌氧的,因此所有硝酸盐-N都应还原为氮气。因此,在生长季节将硝酸盐-N淋溶到地下水中是极不可能的事件。厌氧菌的程度足以溶解铁和锰的氧化物。吸附到这些氧化物表面的有机化学物浸入地下水的风险可能会增加。

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