岩石力学与工程学报
巖石力學與工程學報
암석역학여공정학보
CHINESE JOURNAL OF ROCK MECHANICS AND ENGINEERING
2014年
12期
2539-2545
,共7页
陈存礼%蒋雪%苏铁志%金娟%李文文
陳存禮%蔣雪%囌鐵誌%金娟%李文文
진존례%장설%소철지%금연%리문문
土力学%制样含水率%结构性%压实黄土%无侧限压缩特性%初始结构性参数
土力學%製樣含水率%結構性%壓實黃土%無側限壓縮特性%初始結構性參數
토역학%제양함수솔%결구성%압실황토%무측한압축특성%초시결구성삼수
soil mechanics%molding water content%structure%compacted loess%unconfined compression behaviour%initial structural parameter
对一定试验含水率及干密度下具有不同结构性(排列)的压实黄土试样进行无侧限压缩试验,依据非饱和及饱和压实黄土的应力–应变曲线,定义一个反映压实黄土结构性开始损伤前最大综合结构势的初始结构性参数,研究制样含水率引起的结构性变化对不同试验含水率压实黄土的应力–应变、强度特性及结构性参数的影响。研究结果表明:制样含水率对非饱和压实黄土的结构性及无侧限压缩特性有影响,影响程度随试验含水率的增大而减小,对饱和压实黄土基本没有影响;塑限是一个临界值,试验含水率小于塑限时,影响较大;试验含水率一定时,无侧限抗压强度及初始结构性参数皆随着制样含水率的增大而明显增大,制样含水率一定时,随着试验含水率的增大而明显减小;初始结构性参数可把以试验含水率为参量的无侧限抗压强度与制样含水率关系曲线簇转换为其与初始结构性参数之间的归一化非线性关系,它可以反映制样含水率及试验含水率变化对压实黄土结构性的影响,可以和粒度、密度指标一起合理地描述土的力学性质,具有很好的合理性、灵敏性。
對一定試驗含水率及榦密度下具有不同結構性(排列)的壓實黃土試樣進行無側限壓縮試驗,依據非飽和及飽和壓實黃土的應力–應變麯線,定義一箇反映壓實黃土結構性開始損傷前最大綜閤結構勢的初始結構性參數,研究製樣含水率引起的結構性變化對不同試驗含水率壓實黃土的應力–應變、彊度特性及結構性參數的影響。研究結果錶明:製樣含水率對非飽和壓實黃土的結構性及無側限壓縮特性有影響,影響程度隨試驗含水率的增大而減小,對飽和壓實黃土基本沒有影響;塑限是一箇臨界值,試驗含水率小于塑限時,影響較大;試驗含水率一定時,無側限抗壓彊度及初始結構性參數皆隨著製樣含水率的增大而明顯增大,製樣含水率一定時,隨著試驗含水率的增大而明顯減小;初始結構性參數可把以試驗含水率為參量的無側限抗壓彊度與製樣含水率關繫麯線簇轉換為其與初始結構性參數之間的歸一化非線性關繫,它可以反映製樣含水率及試驗含水率變化對壓實黃土結構性的影響,可以和粒度、密度指標一起閤理地描述土的力學性質,具有很好的閤理性、靈敏性。
대일정시험함수솔급간밀도하구유불동결구성(배렬)적압실황토시양진행무측한압축시험,의거비포화급포화압실황토적응력–응변곡선,정의일개반영압실황토결구성개시손상전최대종합결구세적초시결구성삼수,연구제양함수솔인기적결구성변화대불동시험함수솔압실황토적응력–응변、강도특성급결구성삼수적영향。연구결과표명:제양함수솔대비포화압실황토적결구성급무측한압축특성유영향,영향정도수시험함수솔적증대이감소,대포화압실황토기본몰유영향;소한시일개림계치,시험함수솔소우소한시,영향교대;시험함수솔일정시,무측한항압강도급초시결구성삼수개수착제양함수솔적증대이명현증대,제양함수솔일정시,수착시험함수솔적증대이명현감소;초시결구성삼수가파이시험함수솔위삼량적무측한항압강도여제양함수솔관계곡선족전환위기여초시결구성삼수지간적귀일화비선성관계,타가이반영제양함수솔급시험함수솔변화대압실황토결구성적영향,가이화립도、밀도지표일기합리지묘술토적역학성질,구유흔호적합이성、령민성。
A series of unconfined compression tests were conducted on compacted loess samples with different structures at the same dry density and experimental water content. Based on the stress-strain curves of unsaturated and saturated compacted loess,the initial quantitative parameter was defined to describe the maximum overall structure potential before the start of the structural damage of the compacted loess. The influence of different structures caused by the change of molding water content on the stress-strain and strength characteristics as well as the structural parameter was investigated for the compacted loess with different experimental water contents. The results indicated that the molding water content affected the structure and the unconfined compressibility of unsaturated compacted loess,but had little influence on that of saturated compacted loess. The degree of influence decreased with the increase of water content. The plastic limit was found to be the critical value. When the experimental water content was smaller than the plastic limit,the influence was greater. The unconfined compressive strength and the initial structural parameter increased notably with the increase of the molding water content at the same experimental water content and decreased significantly with the increase of experimental water content at the same molding water content. The group of curves describing the relationships of the unconfined compressive strength versus the molding water content and the experimental water content was normalized into a nonlinear relationship with the initial structural parameter. The normalized nonlinear relationship described the influence of molding water content and experimental water content on the structure of compacted loess. Together with the grain size and the density,it described reasonably the mechanical properties of compacted soil.