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Soil water dynamics and availability for citrus and peanut along a hillslope at the Sunjia Red Soil Critical Zone Observatory (CZO)

机译:孙家红壤临界区天文台山坡土壤水分动态及柑橘和花生的有效性

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The hillslopes of red soils (Ultisols) in southern China are intensively cultivated for cash crops and fruit trees. During the rainy monsoon, soil erosion is prevalent, whereas a summer/autumn dry season induces drought stress. Crops respond differently to these stresses, and have different effects on soil water regime. This study used a combination of field observation and HYDRUS-2D modeling to assess the soil water dynamics and plant available water for peanut (Arachis hypogaea) and citrus (Citrus sinensis) at Sunjia Red Soil Critical Zone Observatory (CZO). Between April 1, 2012 and March 31, 2014, surface runoff and moisture content at 5, 20, 40, and 80 cm depths in the soil under both land uses were monitored at up, middle and foot slope positions along a hillslope. Results indicate that the citrus plot had higher soil water content at 5 cm depth during the dry season, and lower at 20, 40 and 80 cm depths throughout the year than the peanut plot. As expected, the soil water content was higher at foot slope, compared to up slope, and in deeper soil than near surface. We observed limited soil water availability to peanut during mid July to August, and to citrus from mid July to mid-November. Compared to the peanut plot, the citrus plot generally showed 12-28% greater evapotranspiration, 3-4 times less runoff, and 2-57% greater deep drainage. These differences were greater at the up slope position. Our data and HYDRUS-2D simulation suggest that the deep-rooted citrus reduced runoff during the rainy season by increasing macropore flow and canopy interception, and minimized the soil water stress during the dry season by utilizing water from deeper soil. Thus, we recommend trench planting of citrus along with peanut intercropping on hilly red soils as sustainable agricultural practices. (C) 2016 Elsevier B.V. All rights reserved.
机译:中国南部的红色土壤(Ultisols)的山坡上大量种植经济作物和果树。在多雨的季风期间,水土流失很普遍,而夏季/秋季的干旱季节会引发干旱胁迫。作物对这些压力的反应不同,对土壤水分状况的影响也不同。这项研究结合了野外观察和HYDRUS-2D模型,评估了孙家红壤临界区天文台的花生(Arachis hypogaea)和柑桔(Citrus sinensis)的土壤水分动态和植物可用水。在2012年4月1日至2014年3月31日期间,在两种土地利用方式下,分别在山坡的上坡,中坡和脚坡位置监测地表径流和土壤中5、20、40和80厘米深度的水分含量。结果表明,与干旱区相比,旱季柑橘区的土壤水分含量在5 cm处较高,而在20、40和80 cm处较低。不出所料,与上坡相比,在山坡上土壤含水量更高,而在较深的土壤中,土壤含水量高于近地表。我们观察到在7月中旬至8月中花生和从7月中旬至11月中旬对柑橘的土壤水供应有限。与花生田相比,柑橘田通常蒸散量增加了12%至28%,径流减少了3-4倍,深层排水增加了2-57%。这些差异在上坡位置更大。我们的数据和HYDRUS-2D模拟表明,深根柑橘可通过增加大孔流量和冠层截留来减少雨季的径流,并通过利用深层土壤中的水将旱季的土壤水分压力降至最低。因此,我们建议在柑橘丘陵地沟下种植柑橘,并在丘陵的红色土壤上种植花生,作为可持续的农业作法。 (C)2016 Elsevier B.V.保留所有权利。

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