农地耕层与犁底层土壤入渗性能的连续测量方法  

Method for continuously measuring soil infiltrability of plow-cultivated layer and hardpan in farmland

作　　者：孙蓓[1] 马玉莹[1] 雷廷武[1,2] 赵军[2] 啜瑞媛[1] 刘琳[1] 周淑梅[2] 

机构地区：[1]中国农业大学水利与土木工程学院,北京100083 [2]中国科学院水利部水土保持研究所土壤侵蚀与旱地农业国家重点实验室,杨凌712100

出　　处：《农业工程学报》2013年第4期118-124,共7页Transactions of the Chinese Society of Agricultural Engineering

基　　金：国家自然科学基金重点项目(40635027)

摘　　要：研究农田土壤入渗性能对于了解铧式犁耕作对土壤水力性能的影响、指导农地耕作方式决策、农田灌溉、改善农地生态环境具有重要意义。该文提出了一种农耕地耕层与犁底层土壤入渗能力连续测量方法以及相应的计算模型。采用恒定流量向地表供水,由供水在地表湿润面积随时间的变化过程估计地表耕层土壤初期很高的入渗性能,由产流后供水流量与产流流量之差计算相对较低的土壤入渗性能及犁底层土壤入渗性能。并进行了室内模拟试验,结果表明该方法可连续测量农地耕层与犁底层的入渗过程。采用入渗量和供水量对比的方法进行误差分析,相对误差为5.75%,说明该方法具有较高精度。该方法省时、省水便于野外应用,为今后的进一步研究提供手段。The study on farm land infiltration is of great importance for understanding the impacts of plow-cultivation on soil hydrodynamics, guiding cultivation decision making and irrigation as well as improving ecological environments of farm land. A new method, including the experimental system and the related algorithm procedures was advanced for continuous measurement of soil infiltrability curve of cultivated layer and the hardpan of the farm field. A well-controlled water flow of constant flow rate was applied to the soil surface. The initial very high infiltration rate was estimated from the time-dependent function of the wetted soil surface area. And the latter infiltration process, including the relatively steady infiltration of the cultivated layer and that of the hardpan infiltration is estimated from the difference of applied water flow rate and the out flow rate. An integrated experimental system that completely controlled by a computer was developed, including a computer with the supporting software for process control and data record as well as for infiltration process computation, a Mariotte bottle for water supply of constant flow rate, a specially designed outlet unit for point distribution of water flow at the soil surface, a ring for the soil boundary control, a digital camera for automatic record of the increasing process in the wetted soil surface area as time, two electronic balances for measuring the flow rates both of water supply and drainage. Detailed experimental procedures were presented. Computational algorithms for infiltration rates at various steps were detailed. The demonstrational laboratory experiments were conducted to illustrate the experimental procedures, infiltration estimation methods at different stages, using air-dry silty clay with flow rate of about 2 L/h in 3 replicates. The results from the laboratory simulation experiment indicates that this method is capable of making continuous measurement of the infiltration process of typical farm field, including both of the cultivate

关 键 词：入渗 土壤水分 土壤 农地 耕层 犁底层 连续测量 

分 类 号：S152.72[农业科学—土壤学]