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首页> 外文期刊>Annals of the American Thoracic Society >Effects of irrigation and cultivation on the chemical indices of saline-sodic soils in a calcareous environment
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Effects of irrigation and cultivation on the chemical indices of saline-sodic soils in a calcareous environment

机译:灌溉与培养对钙质环境中盐酸盐土壤化学指标的影响

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摘要

Studies on saline-sodic soils have a growing concern during time in many arid and semiarid nations due to human population pressures and need to produce more food and fiber. Nevertheless, little data are available about the quality attributes of the soils when affected by irrigation and cultivation. This study highlights the response of selected chemical indicators of four soil types (Aquic Natrargids, Sodic Aquicambids, Typic Aquisalids, and Typic Halaquepts) associated with calcareous salt-affected soils when changing to cropland. The results revealed a considerable drop in the amounts of soil pH (0.2-0.8 unit), electrical conductivity (69-82%), sodium absorption ratio (62-73%), exchangeable Na (65-90%), and exchangeable sodium percentage (52-69%) following the conversion of saline-sodic soils to cropland, indicating that the processes of desalinization and desodification were promoted by cultivation practices. For the majority of the study soils, an increasing pattern was recorded in the values of organic carbon (15-130%), total N (37-157%), available P (1-7%), exchangeable Ca (20-96%) and Mg (83-94%), and DTPA-extractable Mn (8-85%), Zn (48-85%), Cu (7-75%) with cultivation, whereas the amounts of cation exchange capacity, exchangeable K, available K, and DTPA-extractable Fe were decreased by 1-29, 8-54, 10-60, and 2-54%, respectively. Based on the land productivity index (LPI), 75% of the soils had an increasing trend (a rise of 10-31%) in the LPI [with the improvement of the productive class from average (LPI=20-34) to good class (LPI=35-64)] and 25% had a decreasing pattern (a drop of 10%) after cultivation.
机译:由于人口压力,对许多干旱和半干旱国家的盐水碘土壤的研究具有日益增长的问题,并且需要产生更多的食物和纤维。尽管如此,灌溉和培养影响时,少量数据可以获得土壤的质量属性。该研究突出了四种土壤类型(ABIC Natrargids,Sodic AquicambIds,典型AquiSalids和典型Halaquepts)的所选化学指标的响应在变化到农田时与钙质盐影响的土壤相关。结果表明,土壤pH(0.2-0.8单位),电导率(69-82%),钠吸收率(62-73%),可交换Na(65-90%)和可更换钠的量下降将盐水 - 碳化土壤转化为耕地后的百分比(52-69%),表明培养实践促进了脱盐和去撤代的过程。对于大多数研究土壤,有机碳的值(15-130%),总N(37-157%),可用P(1-7%),可更换Ca(20-96 %)和Mg(83-94%)和DTPA可提取的Mn(8-85%),Zn(48-85%),Cu(7-75%),培养,阳离子交换能力,可兑换K,可用K和DTPA可提取的Fe分别减少1-29,8-54,10-60和2-54%。基于土地生产率指数(LPI),75%的土壤在LPI中具有越来越大的趋势(增长10-31%)[随着从平均(LPI = 20-34)到好的生产课程培养后,25%的阶级(LPI = 35-64)]和25%的模式(滴10%)。

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