广西大学学报(自然科学版)
廣西大學學報(自然科學版)
엄서대학학보(자연과학판)
JOURNAL OF GUANGXI UNIVERSITY (NATURAL SCIENCE EDITION)
2015年
4期
969-977
,共9页
变单向压力%重塑膨胀土%胀限%膨胀变形%线性拟合
變單嚮壓力%重塑膨脹土%脹限%膨脹變形%線性擬閤
변단향압력%중소팽창토%창한%팽창변형%선성의합
variable one-way pressure%restore expansive soil%maximum water content%expansion deformation%linear fitting
为了研究胀限与变单向压力和初始含水率、三向膨胀率与变单向压力和初始含水率的关系,用“膨胀土三向胀缩测试仪”对广西宁明灰白重塑膨胀土进行了三向等压(27 kPa)的情况下变单向压力(27~164 kPa)的膨胀增湿试验。对试验数据进行拟合、对比分析得出:胀限可与变单向压力的对数进行线性拟合,胀限由三向压力决定,与初始含水率无关;无论水平向压力还是竖直向压力,均会抑制该向的膨胀变形,该向膨胀可与该向压力的对数进行一次线性拟合;三向中任一向加压都会同时促进另外两向膨胀变形,该向压力越大,对另外两向膨胀变形的促进作用越大;相同压力条件下,三向膨胀率均与初始含水率呈一次线性负相关;当竖直向压力为水平向压力的2倍时,各向膨胀率与初始含水率关系曲线基本重合。
為瞭研究脹限與變單嚮壓力和初始含水率、三嚮膨脹率與變單嚮壓力和初始含水率的關繫,用“膨脹土三嚮脹縮測試儀”對廣西寧明灰白重塑膨脹土進行瞭三嚮等壓(27 kPa)的情況下變單嚮壓力(27~164 kPa)的膨脹增濕試驗。對試驗數據進行擬閤、對比分析得齣:脹限可與變單嚮壓力的對數進行線性擬閤,脹限由三嚮壓力決定,與初始含水率無關;無論水平嚮壓力還是豎直嚮壓力,均會抑製該嚮的膨脹變形,該嚮膨脹可與該嚮壓力的對數進行一次線性擬閤;三嚮中任一嚮加壓都會同時促進另外兩嚮膨脹變形,該嚮壓力越大,對另外兩嚮膨脹變形的促進作用越大;相同壓力條件下,三嚮膨脹率均與初始含水率呈一次線性負相關;噹豎直嚮壓力為水平嚮壓力的2倍時,各嚮膨脹率與初始含水率關繫麯線基本重閤。
위료연구창한여변단향압력화초시함수솔、삼향팽창솔여변단향압력화초시함수솔적관계,용“팽창토삼향창축측시의”대엄서저명회백중소팽창토진행료삼향등압(27 kPa)적정황하변단향압력(27~164 kPa)적팽창증습시험。대시험수거진행의합、대비분석득출:창한가여변단향압력적대수진행선성의합,창한유삼향압력결정,여초시함수솔무관;무론수평향압력환시수직향압력,균회억제해향적팽창변형,해향팽창가여해향압력적대수진행일차선성의합;삼향중임일향가압도회동시촉진령외량향팽창변형,해향압력월대,대령외량향팽창변형적촉진작용월대;상동압력조건하,삼향팽창솔균여초시함수솔정일차선성부상관;당수직향압력위수평향압력적2배시,각향팽창솔여초시함수솔관계곡선기본중합。
In order to investigate the influence of varying unidirectional pressure and initial water content on the expansion limit and the three-directional swelling ratio, a hygral expansion test for the remolded gray expansive soil from Ningming, Guangxi under varying unidirectional pressure (27~164 kPa) was performed in the condition of equal pressure (27 kPa) in the three directions using the “three-directional swelling shrinkage tester for expansive soil”. Some results are obtained by fit-ting and analyzing the experimental data. The results indicate that the expansion limit is determined by the three-directional pressure, which is irrelevant to the initial water content. The raising of pres-sure in either direction will promote the expansion deformation in other directions, and the expansion deformation can be fitted linearly with the logarithm of the varying unidirectional pressure. The grea-ter the pressure is, the more promotion to the expansion deformation in other two directions will be. Under the same pressure, the three-directional expansion-rate and initial water content was negative-ly related. When the vertical pressure becomes 2 times of the horizontal pressure, the relation curves between the expansion rate and initial water content basically coincides.