磷石膏
碱土
钙质的
磷酸
浸出(土壤学)
石膏
钠吸附比
化学
土壤盐分
导水率
环境化学
灌溉
环境科学
土壤科学
土壤水分
地质学
农学
原材料
生物
古生物学
滴灌
有机化学
作者
Mamoun Abdullah Gharaibeh,Nabil Ibrahim Eltaif,S. H. Shra’ah
标识
DOI:10.1111/j.1475-2743.2010.00260.x
摘要
Abstract Phosphoric acid is increasingly used as a source of water‐soluble P, but it has not been widely tested for its effectiveness in reclaiming calcareous sodic and saline‐sodic soils relative to chemically equivalent rates of gypsum. In lysimeters experiments, we showed that a calcareous saline‐sodic soil can be ‘reclaimed’ using phosphoric acid and leaching with moderately saline irrigation water (sodium adsorption ratio = 4.1 and electrical conductivity = 2.2 dS/m). Phosphoric acid (50% pure) was dissolved directly in the leaching water at application rates of 450, 600 and 900 kg/ha, and phosphogypsum (80% pure) was mixed with soil prior to leaching at application rates of 15, 20, 30 and 40 t/ha. Phosphoric acid was more efficient than the chemical equivalent of phosphogypsum in improving soil hydraulic conductivity, and in reducing the exchangeable sodium percentage (ESP). The ESPs after leaching were: 10 (water only), 5.5–5.3 (phosphoric acid) and 8.2–5.9 (phosphogypsum).
科研通智能强力驱动
Strongly Powered by AbleSci AI