岩土力学
巖土力學
암토역학
ROCK AND SOIL MECHANICS
2010年
1期
15-19,38
,共6页
邵生俊%郑文%王正泓%王帅
邵生俊%鄭文%王正泓%王帥
소생준%정문%왕정홍%왕수
黄土%结构性%构度%无侧限抗压强度
黃土%結構性%構度%無側限抗壓彊度
황토%결구성%구도%무측한항압강도
loess%structure%structure index%uniaxial compressive strength
黄土的结构性是一个重要的物理性质指标,它与土的粒度、密度和湿度一起影响土的力学性质.依据加荷、扰动、浸水释放土结构势的方法,由土的无侧限抗压强度定义了黄土结构性的构度指标.通过多个场地不同黄土的无侧限单轴压缩试验,测试分析了不同含水率原状土、重塑土和饱和原状土的单轴压缩应力-应变曲线及无侧限抗压强度变化规律,由此得出土的构度指标的变化规律.并且,在粒度、密度、湿度相似条件下,比较分析了土的构度指标与其压缩性之间的关系.土的构度指标与粒度、密度和湿度指标一起能够合理描述土的物理力学基本性质.
黃土的結構性是一箇重要的物理性質指標,它與土的粒度、密度和濕度一起影響土的力學性質.依據加荷、擾動、浸水釋放土結構勢的方法,由土的無側限抗壓彊度定義瞭黃土結構性的構度指標.通過多箇場地不同黃土的無側限單軸壓縮試驗,測試分析瞭不同含水率原狀土、重塑土和飽和原狀土的單軸壓縮應力-應變麯線及無側限抗壓彊度變化規律,由此得齣土的構度指標的變化規律.併且,在粒度、密度、濕度相似條件下,比較分析瞭土的構度指標與其壓縮性之間的關繫.土的構度指標與粒度、密度和濕度指標一起能夠閤理描述土的物理力學基本性質.
황토적결구성시일개중요적물이성질지표,타여토적립도、밀도화습도일기영향토적역학성질.의거가하、우동、침수석방토결구세적방법,유토적무측한항압강도정의료황토결구성적구도지표.통과다개장지불동황토적무측한단축압축시험,측시분석료불동함수솔원상토、중소토화포화원상토적단축압축응력-응변곡선급무측한항압강도변화규률,유차득출토적구도지표적변화규률.병차,재립도、밀도、습도상사조건하,비교분석료토적구도지표여기압축성지간적관계.토적구도지표여립도、밀도화습도지표일기능구합리묘술토적물리역학기본성질.
Loess structure is an important physical property, which influences mechanical properties of loess with its particle size, density and humidity. Based on the structure potential of loess released by loading, remolding and saturating, the unconfined compressive strength of intact, remolded and saturated loess were measured by uniaxial compression test; and the structural index of loess was defined by comparing the stability and changeability of loess structure which determined respectively by the ratio of confined compression strength of loess and remolding soil and the ratio of confined compressive strength of saturating loess and loess. Through the unconfined uniaxial compression test of four kinds of loess adopted from different sites, the unconfined uniaxial compression stress-strain curves of intact, remolded and saturated loesses with different water contents were tested to reflect the uniaxial compression stress-strain property, as well as the law of unconfined compressive strength and loess structural index changing with the water content was analyzed for different kinds of loesses. When the particle size, density and humidity of loess being similar, the greater the structure index of loess, the smaller the compressibility and the greater the shear strength of loess. So the structure Index structure together with the particle size, density and humidity can be used to describe reasonably the fundamental physico-mechanical properties of intact soils.