水利学报
水利學報
수리학보
2014年
4期
490-496
,共7页
陶高梁%张季如%庄心善%杨琳
陶高樑%張季如%莊心善%楊琳
도고량%장계여%장심선%양림
土壤%黏粒含量%土-水特征曲线%分形模型
土壤%黏粒含量%土-水特徵麯線%分形模型
토양%점립함량%토-수특정곡선%분형모형
soil%clay content%soil-water characteristic curve%fractal model
土体黏粒含量对土-水特征曲线有重要影响。为了建立描述黏粒含量对土-水特征曲线影响规律的理论模型,本文基于分形理论,建立了质量分维数与黏粒含量的关系式,利用已有试验数据验证了该式的合理性,并从理论上解释了质量分维数随黏粒含量增大的基本规律。在此基础上,结合已有的研究成果,建立了分形模型描述土体黏粒含量对土-水特征曲线影响规律,该模型预测的土-水特征曲线与已有不同土类样本的试验数据吻合较好,从而证明了该模型的有效性。最后,利用该模型同时预测了不同黏粒含量典型土体的土-水特征曲线,阐明了黏粒含量对土-水特征曲线影响的基本规律,即相同吸力条件下,黏粒含量越高,则体积含水率越高。
土體黏粒含量對土-水特徵麯線有重要影響。為瞭建立描述黏粒含量對土-水特徵麯線影響規律的理論模型,本文基于分形理論,建立瞭質量分維數與黏粒含量的關繫式,利用已有試驗數據驗證瞭該式的閤理性,併從理論上解釋瞭質量分維數隨黏粒含量增大的基本規律。在此基礎上,結閤已有的研究成果,建立瞭分形模型描述土體黏粒含量對土-水特徵麯線影響規律,該模型預測的土-水特徵麯線與已有不同土類樣本的試驗數據吻閤較好,從而證明瞭該模型的有效性。最後,利用該模型同時預測瞭不同黏粒含量典型土體的土-水特徵麯線,闡明瞭黏粒含量對土-水特徵麯線影響的基本規律,即相同吸力條件下,黏粒含量越高,則體積含水率越高。
토체점립함량대토-수특정곡선유중요영향。위료건립묘술점립함량대토-수특정곡선영향규률적이론모형,본문기우분형이론,건립료질량분유수여점립함량적관계식,이용이유시험수거험증료해식적합이성,병종이론상해석료질량분유수수점립함량증대적기본규률。재차기출상,결합이유적연구성과,건립료분형모형묘술토체점립함량대토-수특정곡선영향규률,해모형예측적토-수특정곡선여이유불동토류양본적시험수거문합교호,종이증명료해모형적유효성。최후,이용해모형동시예측료불동점립함량전형토체적토-수특정곡선,천명료점립함량대토-수특정곡선영향적기본규률,즉상동흡력조건하,점립함량월고,칙체적함수솔월고。
Clay content of soil has an important influence on soil-water characteristic curve. To establish a theoretical model describing the influence of clay content on soil-water characteristic curve, the relation be-tween the clay content and fractal dimension in terms of mass has been established by means of a fractal theory. This relation was verified by test data and used to explain the basic rule that the fractal dimension increases with the increase of clay content. On this basis, a fractal model which reflects the influence of clay content on soil-water characteristic curve was suggested based on the previous results. The results show that the soil-water characteristic curves predicted by the model are in good agreement with several tests data. The model was applied to predict the soil-water characteristic curves of some soils with different clay content and shows the influence of clay content on the soil-water characteristic curve, i.e., large clay content corresponds to large water content of volume in the case of same soil suction.