水利与建筑工程学报
水利與建築工程學報
수리여건축공정학보
TECHNIQUE OF SEEPAGE CONTROL
2012年
2期
84-87
,共4页
努尔比亚·吾斯曼%何建新%苏枋
努爾比亞·吾斯曼%何建新%囌枋
노이비아·오사만%하건신%소방
含盐量%界限含水率%投影寻踪仿真
含鹽量%界限含水率%投影尋蹤倣真
함염량%계한함수솔%투영심종방진
salt content%boundary moisture content%projection pursuit simulation
土中含盐量影响土的物理力学性能,研究细粒土中总盐含量及不同离子含量(硫酸盐和氯盐)对认识土的界限含水率的影响规律有重要意义。人工配制不同含盐量、不同离子含量的土样,测定土的界限含水率,并运用投影寻踪回归分析方法研究含盐量对土的界限含水率的影响。研究结果表明:加氯化钠时,随着含盐量的增加,土的液、塑限均有下降;加硫酸钠时,随着含盐量的增加,土的液、塑限均有上升,体积发生变化,出现膨胀现象;各加一半时,随着含盐量的增加,土的液限明显下降,塑限变化不大。
土中含鹽量影響土的物理力學性能,研究細粒土中總鹽含量及不同離子含量(硫痠鹽和氯鹽)對認識土的界限含水率的影響規律有重要意義。人工配製不同含鹽量、不同離子含量的土樣,測定土的界限含水率,併運用投影尋蹤迴歸分析方法研究含鹽量對土的界限含水率的影響。研究結果錶明:加氯化鈉時,隨著含鹽量的增加,土的液、塑限均有下降;加硫痠鈉時,隨著含鹽量的增加,土的液、塑限均有上升,體積髮生變化,齣現膨脹現象;各加一半時,隨著含鹽量的增加,土的液限明顯下降,塑限變化不大。
토중함염량영향토적물리역학성능,연구세립토중총염함량급불동리자함량(류산염화록염)대인식토적계한함수솔적영향규률유중요의의。인공배제불동함염량、불동리자함량적토양,측정토적계한함수솔,병운용투영심종회귀분석방법연구함염량대토적계한함수솔적영향。연구결과표명:가록화납시,수착함염량적증가,토적액、소한균유하강;가류산납시,수착함염량적증가,토적액、소한균유상승,체적발생변화,출현팽창현상;각가일반시,수착함염량적증가,토적액한명현하강,소한변화불대。
The influence laws of the total salt content and different ion content(sulfate and chlorine salt) in fine-grained soil to the boundary moisture content of the soil are studied here in detail.Through artificially making the soil samples with different salt content and ion content,the boundary moisture content of the soil is determined,and the influence of salt content on the boundary moisture content of the soil is studied by using projection pursuit regression analysis method.It is found by analysis that when adding sodium chloride,the hydraulic limit and plastic limit of the soil are decreased with salt content increasing,and when adding sodium sulfate,the hydraulic limit and plastic limit of the soil are risen with salt content increasing.At the same time,when size changing,there appears expand phenomenon.When adding each half of the sodium chloride and sodium sulfate,the hydraulic limit of the soil is dropped obviously,and the plastic limit of the soil is changed a little with salt content increasing.