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生物炭對黑土區(qū)土壤水分及其入滲性能的影響
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國家自然科學(xué)基金項(xiàng)目(51479033)、黑龍江省博士后面上資助經(jīng)費(fèi)項(xiàng)目(LBH-Z17017)和東北農(nóng)業(yè)大學(xué)農(nóng)業(yè)農(nóng)村部農(nóng)業(yè)水資源高效利用重點(diǎn)實(shí)驗(yàn)室開放項(xiàng)目(2017009)


Effect of Biochar on Soil Moisture and Its Infiltration Performance in Black Soil Area
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    為探究黑土區(qū)施用生物炭對土壤水分及其入滲性能影響的持續(xù)性,2016—2018年連續(xù)3年在東北黑土區(qū)進(jìn)行了單次施加生物炭(75t/hm2,BC處理)和不施加生物炭(CK處理)的室內(nèi)外對比試驗(yàn),分析各土層土壤含水率及土壤水分入滲過程。結(jié)果表明:施加生物炭可增加各土層土壤含水率,使其極值比Ka和變異系數(shù)Cv減小,且土壤含水率、Ka、Cv的變化幅度均隨生物炭施用年限增加而減弱,2016—2018年苗期耕層土壤含水率增加最多,分別增加了14.54%、11.48%和708%;施加生物炭明顯增大了土壤累積入滲量、土壤入滲速率,增強(qiáng)了土壤入滲能力,促進(jìn)了濕潤鋒的運(yùn)移,各年份BC處理土壤累積入滲量由大到小依次為2016年、2017年、2018年,初始入滲速率f1分別增加了70.48%、58.98%和48.41%,土壤穩(wěn)定入滲速率fc由大到小依次為2016年BC處理(1.65mm/min)、2017年BC處理(1.22mm/min)、2018年BC處理(1.17mm/min)、2016年CK處理(0.46mm/min)、2017年CK處理(0.43mm/min)和2018年CK處理(0.38mm/min);2016—2018年中,2016年BC處理濕潤鋒運(yùn)移距離最深(32.24mm),各表征土壤入滲性能的指標(biāo)均于生物炭施用當(dāng)年效果最優(yōu),而后逐年減弱;土壤累積入滲量與時間具有冪函數(shù)關(guān)系,濕潤鋒運(yùn)移距離與時間具有三次函數(shù)關(guān)系,R2均在0963~0998之間;Philip、Kostiakov、Horton 3個入滲模型擬合對比結(jié)果表明,Kostiakov模型R2最高(0.946~0.991)、RMSE最小(0.516~1.941mm/min),擬合參數(shù)與實(shí)際情況相符,故本研究中Kostiakov模型擬合的土壤水分入滲過程最優(yōu)。本研究可為東北黑土區(qū)施加生物炭后改良土壤水分入滲過程提供理論依據(jù)。

    Abstract:

    In order to explore the persistence of the effects of biochar application on soil moisture and infiltration performance in black soil areas, biochar applied with 75t/hm2 (BC) and without biochar (CK) were carried out for three consecutive years from 2016 to 2018. The indoor and outdoor comparative tests of biochar treatment were carried out to analyze the soil moisture content of various soil layers and the process of soil water infiltration. The results showed that biochar application could make the soil moisture content of each soil layers increase and the extreme value ratio Ka and variation coefficient Cv decrease. And the variation of soil moisture content, Ka and Cv was getting decreased with the increase of biochar application period. From 2016 to 2018, the soil moisture content of the cultivated layer was increased the most, which was increased by 14.54%, 11.48% and 7.08%, respectively. The biochar significantly increased the soil infiltration and soil infiltration rate, enhanced the soil infiltration capacity and promoted the migration of the wet peaks. The order of soil infiltration in the BC group from 2016 to 2018 was 2016, 2017 and 2018, and the initial infiltration rate f1 was increased by 70.48%, 58.98% and 48.41%. The stable infiltration rate fc was 2016 BC treatment (1.65mm/min), 2017 BC treatment (1.22mm/min), 2018 BC treatment (1.17mm/min), 2016 CK treatment (0.46mm/min),2017 CK treatment (0.43mm/min) and 2018 CK treatment (0.38mm/min). And the 2016 BC treatment humid peak was the deepest in 2016 to 2018 at 32.24mm. The indexes indicating that soil infiltration performance was the best in the year of biochar application and then weakened year by year. The soil infiltration amount had a good power function relationship with time. The wet peak migration distance and time had a good cubic function relationship, R2 was between 0963 and 0998. Comparing the fitting results of three infiltration models of Philip, Kostiakov and Horton models, Kostiakov model had the highest R2 value (0.946~0.991) and the smallest RMSE (0.516~1.941mm/min). There was no phenomenon that the fitting parameters were inconsistent with the actual situation, also. In the case of this study, the soil water infiltration process was optimal by Kostiakov model. The results provided a theoretical basis for improving the soil water infiltration process after applying biochar in the black soil region of Northeast China.

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魏永霞,王鶴,劉慧,吳昱.生物炭對黑土區(qū)土壤水分及其入滲性能的影響[J].農(nóng)業(yè)機(jī)械學(xué)報,2019,50(9):290-299. WEI Yongxia, WANG He, LIU Hui, WU Yu. Effect of Biochar on Soil Moisture and Its Infiltration Performance in Black Soil Area[J]. Transactions of the Chinese Society for Agricultural Machinery,2019,50(9):290-299.

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  • 收稿日期:2019-01-02
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  • 在線發(fā)布日期: 2019-09-10
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