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農(nóng)膜殘留對(duì)砂壤土和砂土水分入滲和蒸發(fā)的影響
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內(nèi)蒙古自然科學(xué)基金項(xiàng)目(2016JQ06)、國(guó)家自然科學(xué)基金項(xiàng)目(51669020、51539005、51469022)、內(nèi)蒙古科技計(jì)劃項(xiàng)目和內(nèi)蒙水利科技計(jì)劃項(xiàng)目


Effects of Residual Plastic Film on Infiltration and Evaporation for Sandy Loam and Sandy Soil
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    摘要:

    通過室內(nèi)試驗(yàn)設(shè)置5個(gè)不同殘膜量(0、50、100、200、400kg/hm2)處理,研究不同殘膜量對(duì)砂壤土和砂土水分入滲濕潤(rùn)鋒、入滲速率、累積入滲量、土壤累積蒸發(fā)量和蒸發(fā)速率的影響,并評(píng)價(jià)了主要土壤入滲、蒸發(fā)模型在農(nóng)膜殘留土壤的適用性。結(jié)果表明:隨著土壤中殘膜量增多,砂壤土和砂土入滲速率變慢,土壤濕潤(rùn)鋒運(yùn)移相同距離所需時(shí)間均顯著增加,其中運(yùn)移30cm時(shí),砂壤土殘膜量400kg/hm2處理(SL5)比無殘膜處理(SL1)運(yùn)移時(shí)間增加了27.56%;相同入滲時(shí)間內(nèi)累積入滲量隨殘膜量增加均顯著減?。≒<0.05),入滲結(jié)束后SL5處理比SL1處理累積入滲量減小了52.01mL(23.12%);殘膜量增加導(dǎo)致蒸發(fā)速率、累積蒸發(fā)量都顯著減?。≒<0.05),蒸發(fā)結(jié)束后SL5處理比SL1處理累積蒸發(fā)量減小了30.63%,且不同殘膜量對(duì)砂壤土的影響大于砂土。對(duì)4個(gè)土壤水分入滲及蒸發(fā)模型進(jìn)行擬合,結(jié)果顯示Kostiakov和Philip入滲模型均能較好模擬殘膜條件下土壤水分入滲,其中Philip入滲模型擬合精度高于Kostiakov入滲模型,且對(duì)砂土中農(nóng)膜殘留下的土壤水分入滲模擬效果更好;Black蒸發(fā)模型隨著殘膜量增加擬合精度下降,而Rose蒸發(fā)模型受殘膜量的影響較小,更適合于農(nóng)膜殘留土壤累積蒸發(fā)量估算。

    Abstract:

    The residual plastic film seriously affected the soil water infiltration and evaporation. Five residual plastic film treatments were conducted to study the effects of different residual plastic film amounts (0kg/hm2,50kg/hm2, 100kg/hm2, 200kg/hm2 and 400kg/hm2) on soil water infiltration and evaporation characteristics, and the infiltration front, infiltration rate, cumulative infiltration, cumulative evaporation and the evaporation rate were mainly studied based on the different residual plastic film quantities for sandy loam and sandy soil, and then the performance of main soil infiltration and evaporation model with residual plastic film was evaluated. The results showed that with the increase of residual plastic film quantity in the soil, the infiltration rates of sandy loam and sandy soil were decreased slowly, the time required for wetting front migration was increased significantly, and the sandy loam with 400kg/hm2 residual plastic film treatment (SL5) was increased by 27.56% compared with that of nonresidual plastic film treatment (SL1) at 30cm soil layer. In addition, the cumulative infiltration amount was significantly decreased (P<0.05) in the same infiltration time, and the cumulative infiltration amount of SL5 treatment was reduced by 52.01mL (23.12%) compared with SL1 at the end of infiltration. The evaporation rate and cumulative evaporation were significantly reduced (P<0.05) with the increase of residual plastic film quantity, the cumulative evaporation rate of SL5 treatment was 30.63% less than that of SL1 after evaporation, and the influence of different residual plastic film amounts on sandy loam was greater than that of sandy soil. The four major soil water infiltration and evaporation model were evaluated, it was showed that both Kostiakov and Philip infiltration models can well simulate the soil water infiltration for the soil with residual plastic film, but the Philip model had better performance than Kostiakov model, and had better adaptability for sandy soil with plastic film residue. The fitting accuracy of Black evaporation model was decreased with the increase of residual plastic film quantity, but the Rose evaporation model was less influenced by the amount of residual plastic film. So it can be concluded that the Rose evaporation model was more suitable for the plastic film residual soil cumulative evaporation estimation.

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王志超,李仙岳,史海濱,張棟良,徐鵬程.農(nóng)膜殘留對(duì)砂壤土和砂土水分入滲和蒸發(fā)的影響[J].農(nóng)業(yè)機(jī)械學(xué)報(bào),2017,48(1):198-205. WANG Zhichao, LI Xianyue, SHI Haibin, ZHANG Dongliang, XU Pengcheng. Effects of Residual Plastic Film on Infiltration and Evaporation for Sandy Loam and Sandy Soil[J]. Transactions of the Chinese Society for Agricultural Machinery,2017,48(1):198-205.

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  • 收稿日期:2016-05-20
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  • 在線發(fā)布日期: 2017-01-10
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