又称“漠土”。漠境地区发育的地带性土壤。广泛分布于温带和热带漠境地区，非洲、大洋洲、中亚、北美、南美均有分布，约占地球陆地面积的10%。
荒漠土壤（desert soil）是指在干旱荒漠条件下形成的土壤。广泛分布于温带和热带漠境地区，非洲、大洋洲、中亚、北美、南美均有分布，约占地球陆地面积的...
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Desert soil clay contents were very low (below 10% averagely), soil texture was silt loam or sandy loam.
主要研究结论如下:1.荒漠土壤粘粒含量很低(平均在10%以下),质地为粉壤或砂壤。
参考来源 - 开垦对荒漠土壤性状的影响So we can reach the conclusion that S. javanicum can be considered as a pioneer in the improvement of desert soil.
因此我认为在改良荒漠土壤时，蓝藻门伪枝藻属的S. javanicum可以作为先锋物种。
参考来源 - 吉林省伪枝藻属（Scytonema）的研究·2,447,543篇论文数据，部分数据来源于NoteExpress
本文通过模拟降雨及降雨后自然条件下的土壤表面水分蒸发，研究了粉煤灰和城市污泥改良荒漠土壤对持水性能的影响。
To study the water-holding capacities of desert soil and the soil improved with coal ash and sewage sludge, experiments were designed to simulate rainfall and natural evaporation.
本文通过模拟降雨及降雨后自然条件下的土壤表面水分蒸发，研究了粉煤灰和城市污泥改良荒漠土壤对持水性能的影响。
To study the water-holding capacities of desert soil and the soil amended with coal ash and sewage sludge, experiments were designed to simulate rainfall and natural evaporation.
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