Department of Soil and Water Sciences and The Seagram Center for Soil and Water Sciences, The Hebrew University, P.O. Box 12, 76100, Rehovot, Israel.
Environ Monit Assess. 1995 Jan;37(1-3):17-37. doi: 10.1007/BF00546878.
Secondary salinization of intensively irrigated lands is an increasingly alarming redesertification process experienced in many irrigated regions of the developed countries. The major cause is a profound interference in the geochemical/salt balances of irrigated regions. A case-in-point is the recent salinization of the Yizre'el Valley, a 20,000 ha intensively irrigated region in Israel. The extremely intensive and advanced agroecosystem developed in the region since the 1940s included pumping and importing irrigation water by the National Water Carrier, large-scale reclamation and reuse of municipal sewage water, winter flood impoundment in reservoirs for summer irrigation, and cloud seeding to enhance rainfall. Modern irrigation methods were applied, including sprinkler, trickle, moving-line, and center-pivot systems. Water use efficiency at any level was very high. Nevertheless, large-scale salinization of regional water resources and many fields had developed in the mid-1980s. Reconstructing and evaluating the water and salt balances of the Yizre'el Valley (using Cl as the representative salt constituent) shows that as water use in the valley increased to about 60 million m(3) per year, the importing of soluble salts by water totaled 15,000 tons of Cl per year. Recirculated salt - salt picked up by impounded surface water and applied to fields - increased significantly and in the late 1980s amounted to more than 9,000 tons Cl per year. The source of recirculated salts was the accumulated salts in soils and in the shallow aquifer in the valley, which were leached by floodwater or drained or infiltrated into reservoirs, grossly and adversely affecting water quality. Analysis of the Yizre'el Valley's case points to the utmost importance of maintaining the geochemical balances in addition to increasing irrigation efficiency. An irrigated region may achieve geochemical balance by the following means: limiting the extent of irrigated areas, developing a well-maintained drainage system that drains tail-water and salinized shallow-aquifer water, and devoting a significant portion of water for regional leaching. The sustained long-term productivity of irrigated lands in arid zones crucially depends on correctly managing water and soil resources. Regional management of irrigated lands to prevent secondary desertification will be aimed at carefully balancing the undisputed benefits of irrigation with the long-term (on time scales of 10 to 100 years) detrimental processes set in motion when irrigation is introduced to arid and semiarid zone soils.
集约化灌溉土地的次生盐渍化是许多发达国家灌溉区日益严重的荒漠化过程。主要原因是对灌溉区地球化学/盐分平衡的严重干扰。一个典型的例子是最近以色列 2 万公顷集约化灌溉的 Yizre'el 流域的盐渍化。自 20 世纪 40 年代以来,该地区发展了极其密集和先进的农业生态系统,包括国家水道的抽水和引水灌溉、大规模开垦和再利用城市污水、冬季洪水在水库中蓄积以供夏季灌溉以及人工增雨以增加降雨量。采用了现代灌溉方法,包括喷灌、滴灌、移动线和中心枢轴系统。任何层面的水利用效率都非常高。然而,到 20 世纪 80 年代中期,该地区的水资源和许多农田已经出现了大规模的盐渍化。对 Yizre'el 流域的水盐平衡进行重建和评估(以 Cl 作为代表性盐分)表明,随着流域用水量增加到每年约 6000 万立方米,水带入的可溶性盐分每年总计 1.5 万吨 Cl。再循环盐——由蓄水地表水收集并应用于农田的盐分——显著增加,到 20 世纪 80 年代末,每年超过 9000 吨 Cl。再循环盐的来源是流域土壤和浅层含水层中积累的盐分,这些盐分被洪水淋滤或排水或渗透到水库中,严重影响了水质。对 Yizre'el 流域案例的分析指出,除了提高灌溉效率外,维持地球化学平衡至关重要。灌溉区可以通过以下方式达到地球化学平衡:限制灌溉面积、开发维护良好的排水系统,排出尾水和盐化浅层含水层水,以及将大量水资源用于区域淋洗。干旱区灌溉土地的持续长期生产力取决于对水土资源的正确管理。为防止次生荒漠化而对灌溉土地进行区域管理,将旨在仔细平衡灌溉带来的无可争议的好处与引入干旱和半干旱区土壤的长期(在 10 至 100 年的时间尺度上)不利过程。