1. 哈尔滨工业大学 深圳研究生院深圳市城市与土木工程防灾减灾重点试验室,广东,深圳,518055
2. 河海大学 岩土力学及堤坝工程教育部重点实验室,南京,210098
3. 广州市香港科大霍英东研究院,广州,511458
4. 香港科技大学 土木及环境工程学系,香港
网络首发:2013-10-18,
纸质出版:2013
移动端阅览
陈 锐, 刘 坚, 吴宏伟, 等. 一种装配式新型张力计的研制[J]. 岩土力学, 2013,34(10).
CHEN Rui, LIU Jian, NG C W W, et al. Development of a new fabricated tensometer[J]. 2013, 34(10).
土体干湿过程引发的岩土工程问题已逐渐受到重视。通常采用张力计量测80 kPa以内的土体吸力,并将其应用于边坡失稳等岩土工程问题的分析中。然而,传统张力计由于内部腔体体积过大且结构复杂,造成张力计难以饱和,吸力量测时反应时间长,并易发生汽化,严重影响其可靠性和灵敏性。为弥补传统张力计的设计缺陷,提出了一种装配式新型张力计。该张力计内腔结构简单且体积小。饱和前先拆分张力计再分别饱和其主要部件,最后重新装配。此设计简化了饱和程序并提高了效率。通过对比传统张力计和新型张力计的性能,证实了新型张力计具有更强的汽化持久性,其吸力量测的灵敏性和可靠性得到了显著的提高。标定试验表明,相比于传统张力计,新型张力计的灵敏性提高了90%。测量-80 kPa的孔隙水压力时,新型张力计的平衡时间为1.5 min,仅占传统张力计反应时间的10%。相同的测量条件下,传统张力计的测量误差为30%,而新型张力计的测量误差仅为0.7%。
Ever more attention has been paid to geotechnical problems induced by wetting and drying of soils recently. Suction up to 80 kPa
measured by tensometers
has been used for analyzing geotechnical problems such as slope instability during wetting and drying. However
existing tensometer generally has a long response time and is easy to cavitate since it has a large volume of water reservoir and complicated internal structure. These drawbacks affect the sensitivity and reliability of a conventional tensometer seriously. In order to overcome these shortcomings
a newly developed fabricated tensometer is introduced. This type of new tensometer with fabricated structure has a simple internal structure and a small volume of water reservoir. At the same time
a drainage hole is introduced to prevent large excess pore water pressure during the process of reassembling. More importantly
its saturation procedure is simple and efficient since the high air-entry ceramic disc and pore pressure transducer of this new tensometer can be disassembled for saturation separately and effectively. After the saturation of the high air-entry ceramic disc and pore pressure transducer
these key components are reassembled together as a tensometer ready for use. As compared with a conventional tensometer
the sensitivity and reliability of this new tensometer are justified. The results of calibration test show that the sensitivity of the new tensometer increases by 90% by comparing with the conventional tensometer. In the case of measuring the pore water pressure of -80 kPa
the equilibrium time required for this new tensometer is only 1.5 minite
about 10% of that for the conventional tensiometer. Moreover
the reliability of the new tensometer is better than that of the conventional tensometer. The measurement error of the conventional tensiometer is about 30%
when measuring the pore water pressure of -80 kPa. Subjected to the same conditions
the new tensometer shows a measurement error of only 0.7%.
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