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生物炭對(duì)草甸黑土物理性質(zhì)及雨后水分動(dòng)態(tài)變化的影響
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國(guó)家自然科學(xué)基金項(xiàng)目(51479033),、“十二五”國(guó)家科技支撐計(jì)劃項(xiàng)目(2014BAD12BO1)和東北農(nóng)業(yè)大學(xué)博士基金項(xiàng)目(2010RCB65)


Influences of Biochar on Physical Properties of Meadow Black Soil and Dynamic Changes of Soil Water after Individual Rainfall
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    摘要:

    為探明生物炭對(duì)草甸黑土物理性質(zhì)及雨后水分動(dòng)態(tài)變化的影響,,在大豆全生育期生長(zhǎng)條件下,研究了東北黑土區(qū)草甸黑土5種生物炭添加量(0,、25,、50,、75、100t/hm)下土壤物理性質(zhì)(包括:土壤水分特征曲線,、土壤含水率常數(shù),、土壤水分?jǐn)U散率)和單次降雨土壤含水率變化特征,分析了生物炭對(duì)黑土區(qū)草甸黑土耕層土壤持水能力及雨后水分動(dòng)態(tài)變化的影響,。結(jié)果表明,,施用生物炭能降低土壤殘余含水率,增加土壤飽和含水率和田間持水量,,其中對(duì)殘余含水率的影響最顯著,,100t/hm生物炭處理使殘余含水率最多降低27.6%;施用生物炭能明顯降低土壤水分?jǐn)U散率,,隨生物炭添加量的增加依次比對(duì)照組減少34.8%,、37.5%、71.4%和58.9%,;在單次降雨過(guò)程中,,施用生物炭能減小土壤含水率的變化幅度,使土壤含水率在降雨之后更快地由迅速下降期進(jìn)入緩慢下降期,,并能明顯提高緩慢下降期對(duì)應(yīng)的土壤含水率,;施用生物炭可以提高大豆產(chǎn)量,以75t/hm生物炭處理最高,。研究結(jié)果可為黑土區(qū)農(nóng)業(yè)水土資源高效利用與保護(hù)提供理論依據(jù),。

    Abstract:

    The effects of biochar which was made of crop straw on physical properties of meadow black soil and dynamic changes of soil water after individual rainfall were studied. The experiments were conducted by field pilots which were located at the sloping farm-land with three degrees of land slope gradient of Hongxing State Farm, Heilongjiang Province in 2015, and soybean, the main crop type of study area, was selected as experimental crop. Five levels of biochar were set, as 0t/hm, 25t/hm, 50t/hm, 75t/hm and 100t/hm of biochar were put in the field pilots, which were represented by CK, C1, C2, C3 and C4, respectively. During the whole growth period of soybean, the soil physicochemical properties were investigated, including soil water characteristic curve, soil water diffusivity, soil bulk density, rate of soil porosity, organic matter content of soil, saturated soil water content, field water capacity and characteristics of soil water after individual rainfall. Soil water characteristic curve was measured by centrifuge, soil water diffusivity was tested by horizontal vitreous soil column, and soil water contents were measured by TDR field soil water measurement system in situ. The results showed that biochar could remarkably reduce soil bulk density and decrease soil water diffusivity of meadow black soil in the black soil area. The residual soil water content could be declined by 27.6% by treatment of C4. With the increase of biochar quantitative level, soil water diffusivities of C1, C2, C3 and C4 were decreased by 34.8%, 37.5%, 71.4% and 58.9%, respectively. Additionally, it could give a rise to the saturated soil water content, field capacity and soybean yield, and the treatment with 75t/hm biochar got the highest yield. During an individual rainfall, with the use of biochar, the variation amplitude of soil water content tended to fall. This helped to accelerate the process of soil water content changing from rapid declining stage to slow declining stage, meanwhile, it increased the soil water content in the slow declining stage obviously. The research results can provide theoretical foundation for efficient utilization and protection of soil and water resources in agriculture in the black soil region.

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魏永霞,劉志凱,馮鼎銳,孫繼鵬,張雨鳳.生物炭對(duì)草甸黑土物理性質(zhì)及雨后水分動(dòng)態(tài)變化的影響[J].農(nóng)業(yè)機(jī)械學(xué)報(bào),2016,47(8):201-207. Wei Yongxia, Liu Zhikai, Feng Dingrui, Sun Jipeng, Zhang Yufeng. Influences of Biochar on Physical Properties of Meadow Black Soil and Dynamic Changes of Soil Water after Individual Rainfall[J]. Transactions of the Chinese Society for Agricultural Machinery,2016,47(8):201-207.

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  • 收稿日期:2015-12-12
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  • 在線發(fā)布日期: 2016-08-10
  • 出版日期: 2016-08-10
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