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首页> 外文期刊>Agricultural Water Management >Detecting soil salinity changes in irrigated Vertisols by electrical resistivity prospection during a desalinisation experiment.
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Detecting soil salinity changes in irrigated Vertisols by electrical resistivity prospection during a desalinisation experiment.

机译:在脱盐实验中通过电阻率前景检测灌溉的Vertisol中的土壤盐分变化。

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Increasing soil salinity threatens the sustainability of irrigation schemes in several rice growing areas of the world, particularly in western Africa. Desalinisation is needed to sustain irrigated rice cultivation. However, to keep track of the effectiveness of any desalinisation method, monitoring of soil salt content is required. The objective of this study was to assess the ability of non-destructive electrical resistivity prospection to monitor salinity changes (spatial and temporal) in a Vertisol profile during a desalinisation experiment in Kollo, Niger. Desalinisation was induced by successive ponding and flushing cycles on a 10 m x 10 m square plot. Seven data acquisition campaigns were performed between July 13 and September 24 2009. In each campaign, (i) apparent electrical resistivity measurements were performed with two electrode spacings (10 and 30 cm) and were transformed into the inverse apparent electrical conductivity (ECa), (ii) soil samples were extracted from three soil layers (0-10, 10-20, and 20-40 cm). Desalinisation was more efficient for the topsoil layer than for the deeper ones. Mean electrical conductivity of 1:5 aqueous extract of soil samples (EC) decreased from initial values of 2.0, 2.8 and 2.9 dS m-1 to 1.3, 2.2 and 2.6 dS m-1 respectively at 0-10, 10-20 and 20-40 cm. The relative decrease in salt stocks was estimated at 35.7, 22.7 and 11.4% of the initial amounts in these respective soil layers. Mean ECa measured at the soil surface also decreased over time, and the highest correlation (R=0.57) was observed between ECa30 cm and EC of the upper soil layer (0-10 cm). ECa survey allowed the detection of spatial and temporal salinity changes with a high spatial resolution. Relative decrease in ECa over time was an indicator of the desalinisation process. This appears useful to adjust water supply for saline soil reclamation, particularly in regions with high water scarcity.
机译:土壤盐分的增加威胁着世界几个水稻种植地区(特别是在西部非洲)的灌溉计划的可持续性。为了保持灌溉水稻的种植,需要进行脱盐处理。但是,为了跟踪任何脱盐方法的有效性,需要监测土壤盐分含量。这项研究的目的是评估在尼日尔Kollo进行的脱盐实验中,非破坏性电阻率前景监测Vertisol剖面中盐度变化(空间和时间)的能力。通过在10 m x 10 m的正方形图上进行连续的冲洗和冲洗循环来诱导淡化。在2009年7月13日至9月24日之间进行了7次数据采集活动。(i)在两个电极间距(10和30 cm)下进行视电阻率测量,并将其转换为反视电导率(ECa), (ii)从三个土壤层(0-10、10-20和20-40 cm)中提取土壤样品。表层土壤的脱盐处理比深层土壤的脱盐处理更为有效。 1:5的土壤样品水提取物(EC)的平均电导率从2.0、2.8和2.9 dS m -1 的初始值降低到1.3、2.2和2.6 dS m -1 < / sup>分别位于0-10、10-20和20-40厘米处。在这些相应的土壤层中,盐储量的相对减少量估计分别为初始数量的35.7%,22.7%和11.4%。在土壤表面测得的平均ECa随时间也下降,在上部土壤层ECa 30 cm 与ECa之间的相关性最高( R = 0.57)(0 -10厘米)。 ECa调查允许以高空间分辨率检测时空盐度变化。 ECa随时间的相对减少是脱盐过程的指标。这似乎对于调节盐碱土壤开垦的供水很有用,特别是在缺水率高的地区。

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