| 降雨-径流过程中土壤表层磷迁移过程的模拟研究 |
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| 引用本文： | 单保庆,尹澄清,于静,白颖.降雨-径流过程中土壤表层磷迁移过程的模拟研究[J].环境科学学报,2001,21(1):7-12. |
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| 作者姓名： | 单保庆 尹澄清 于静 白颖 |
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| 作者单位： | 1. 中国科学院生态环境研究中心
2. 合肥市环境监测站, |
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| 基金项目： | 国家自然科学基金资助项目 !(4 97710 6 7) |
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| 摘 要： | 以人工降雨的方法，对巢湖边旱作表层土壤在降雨后所产生的磷迁移过程进行了研究，结果表明：在两种雨强植（70mm和35mm）90min内模拟的降雨过程中，供试的土壤产生两种径流模式：表面径流和土壤内部培中流，降雨强度大，表面径流和壤中流始流时间早，水流量和深度相应高，累积输出也多，相同雨强下，农田作物的覆盖作用胡促进壤中流，减缓表面流，但对始流时间的影响不大，4种模拟土类型的表面径流累积输出的大小顺序为：BN70（降雨量70mm，盖度为0）＞BC70（降雨量70mm，盖度为80％）＞BN35（降雨量35mm，盖度为０）＞ＢＣ３５（降雨量７０mm，盖度为０）＞ＢＣ７０（降雨量７０mm，盖度为８０％）＞ＢＮ３５（降雨量３５mm，盖度为０）＞ＢＣ３５（降雨量35mm,盖度为８０％），培中流的量序为：ＹＣ７０＞ＹＮ７０＞ＹＣ３５＞ＹＮ３５，裸露土壤的总磷浓度曲线呈波浪状递减，作物覆盖土壤则呈均匀缓慢的递减趋势，土壤物理结构和作特特征对溶解性总磷的变化趋势起主导作用，在中到大雨条件下，壤中累积输出的径流量都低于表面流，差幅决定于土培表层界面特征，表面径流中的磷迁移量是土壤中流的３－４倍。
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| 关 键 词： | 降雨模拟 表面径流 磷迁移 过程模拟 表面土壤 |
| 文章编号： | 0253-2468(2001)-01-0007-06 |
| 收稿时间： | 1999/12/13 0:00:00 |
| 修稿时间： | 2000/3/24 0:00:00 |
Study on phosphorus transport in the surface layer of soil with rainfall simulation method |
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| SHAN Baoqing,YIN Chengqing,YU Jing and BAI Ying.Study on phosphorus transport in the surface layer of soil with rainfall simulation method[J].Acta Scientiae Circumstantiae,2001,21(1):7-12. |
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| Authors: | SHAN Baoqing YIN Chengqing YU Jing and BAI Ying |
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| Affiliation: | SKLEAC, Research Center for Eco-Environmental Sciences, Chinese Academy of Sciences, Beijing 100085,SKLEAC, Research Center for Eco-Environmental Sciences, Chinese Academy of Sciences, Beijing 100085,The Environmental Monitor Station of Hefei, Anhui Province, 230031 and The Environmental Monitor Station of Hefei, Anhui Province, 230031 |
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| Abstract: | The phosphorus transport in the crop soil within Liuchahe watershed was studied with rainfall simulation method. The results showed that, under two simulated rainfall intensities (precipitation 70?mm and 35?mm,within 90?minutes), there were two runoff forms: surface runoff and subsurface runoff. The water flow volume and phosphorus concentration in both runoffs increased with the rainfall intensity improved; during the same rainfall event, the coverage of crop increased the process of subsurface runoff and impeded the surface runoff. The TP concentration change of soil with no crop coverage exported declinedly in a wavy way, but it showed an equable decline when crop existed. The crop coverage and soil porosity influenced the concentration variation of the dissolved phosphorus (DP), especially in the subsurface runoff. The water volume of surface runoff was less than the subsurface runoff in both events, and the export difference of phosphorus between two runoff types during the same rainfall event was 3 to 4 times. |
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| Keywords: | Rainfall simulation surface runoff subsurface runoff phosphorus transport |
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