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土壤表層含水率與鎮(zhèn)壓力作用下探針貫入阻力變化規(guī)律
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國家自然科學(xué)基金項(xiàng)目(32401710)、國家重點(diǎn)研發(fā)計(jì)劃項(xiàng)目(2023YFD1500401)、興安盟本級(jí)科技合作項(xiàng)目和中國農(nóng)業(yè)大學(xué)2115人才工程項(xiàng)目


Variation of Probe Penetration Resistance under Soil Surface Moisture Content and Compaction Pressure
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    摘要:

    針對(duì)多數(shù)研究需單獨(dú)測量單個(gè)土壤參數(shù)、對(duì)貫入阻力(PR)響應(yīng)多參數(shù)研究較少等問題,本文以粘壤土為研究對(duì)象,開展土壤含水率和鎮(zhèn)壓力對(duì)探針貫入阻力的影響研究。設(shè)置6個(gè)含水率和3個(gè)鎮(zhèn)壓力,記錄各條件下探針貫入土壤過程中的阻力變化曲線。以探針貫入曲線終峰值(FP)、相對(duì)波動(dòng)帶寬(RFBW)和探針貫入阻力曲線傅里葉能量(PRFE)為指標(biāo)進(jìn)行全因素試驗(yàn)。結(jié)果表明:對(duì)于上升效應(yīng),當(dāng)土壤含水率從0增至10%時(shí),隨著含水率增加,終峰值不斷提高,含水率10%時(shí)達(dá)到最大值2.492N(較0增加230.94%);鎮(zhèn)壓力在低含水率時(shí)對(duì)終峰值影響較大,高含水率時(shí)影響減弱。對(duì)于波動(dòng)特性,當(dāng)含水率為0~15%時(shí),相對(duì)波動(dòng)帶寬和探針貫入阻力曲線傅里葉能量均隨含水率增加而下降,含水率15%時(shí)相對(duì)波動(dòng)帶寬降幅為含水率0時(shí)的68.05%,探針貫入阻力曲線傅里葉能量降至含水率0時(shí)的85.80%;隨著鎮(zhèn)壓力增加,相對(duì)波動(dòng)帶寬與探針貫入阻力曲線傅里葉能量均下降,鎮(zhèn)壓力75kPa時(shí)相對(duì)波動(dòng)帶寬降至鎮(zhèn)壓力15kPa時(shí)的74.62%,探針貫入阻力曲線傅里葉能量降為鎮(zhèn)壓力15kPa時(shí)的87.37%。研究結(jié)果揭示了土壤含水率和鎮(zhèn)壓力對(duì)探針貫入阻力的影響規(guī)律,為研發(fā)土壤性質(zhì)測試裝置提供了基礎(chǔ)。

    Abstract:

    Aiming at the problems that most studies required the individual measurement of single soil parameters and there were few studies on the response of multiple parameters to the penetration resistance (PR), taking the clay loam as the research object and a study on the influence of soil moisture content and compaction pressure on the PR was conducted. Six moisture contents and three compaction pressures were set, and the resistance change curves during the process of the probe penetrating the soil under various conditions were recorded. A full-factor experiment was carried out with the final peak (FP) of the probe penetration curve, the relative fluctuation bandwidth (RFBW), and the Fourier energy of the probe penetration resistance curve (PRFE) as the indicators. The results showed that for the ascending effect, when the soil moisture content was increased from 0 to 10%, with the increase of the moisture content, FP was continuously increased, and reached the maximum value of 2.492N at a moisture content of 10% (an increase of 230.94% compared with 0); the compaction pressure had a greater impact on FP at low moisture content, and the impact weakened at high moisture content. For the fluctuation characteristics, when the moisture content was between 0 and 15%, both RFBW and PRFE were decreased with the increase of the moisture content. At a moisture content of 15%, the decrease rate of RFBW was 68.05% of that at a moisture content of 0, and PRFE dropped to 85.80% of that at a moisture content of 0; with the increase of the compaction pressure, both RFBW and PRFE were decreased. When the compaction pressure was 75kPa, the RFBW dropped to 74.62% of that when the compaction pressure was 15kPa, and PRFE dropped to 87.37% of that when the compaction pressure was 15kPa. The research results revealed the influence law of soil moisture content and compaction pressure on the probe PR, providing a basis for the development of soil property testing devices.

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王志楠,盧彩云,何進(jìn),王慶杰,賀棟,王泉玉.土壤表層含水率與鎮(zhèn)壓力作用下探針貫入阻力變化規(guī)律[J].農(nóng)業(yè)機(jī)械學(xué)報(bào),2025,56(6):167-176,204. WANG Zhinan, LU Caiyun, HE Jin, WANG Qingjie, HE Dong, WANG Quanyu. Variation of Probe Penetration Resistance under Soil Surface Moisture Content and Compaction Pressure[J]. Transactions of the Chinese Society for Agricultural Machinery,2025,56(6):167-176,204.

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  • 收稿日期:2025-05-06
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  • 在線發(fā)布日期: 2025-06-10
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