5.1 This test method can be used to determine the density and water content of naturally occurring soils and of soils placed during the construction of earth embankments, road fills, and structural backfills.
5.2 Time domain reflectometry (TDR) measures the apparent dielectric constant (Procedure A) and the apparent dielectric constant, first voltage drop and long term voltage (V1 and Vf) (Procedure B) of soil. The apparent dielectric constant is affected significantly by the water content and density of soil, and to a lesser extent by the chemical composition of soil and pore water, and by temperature. The first voltage drop and long term voltage (V1 and Vf) are affected significantly by the water content, density, and the chemical composition of the in situ pore water, and to a lesser extent the chemical composition of the soil solids. This test method measures the gravimetric water content and makes use of a different relationship between the electrical properties and water content from Test Method D6565 which measures the volumetric water content.
5.3 Soil and pore water characteristics are accounted for in Procedure A with two calibration constants and for Procedure B with five calibration constants. The two soil constants for Procedure A are determined for a given soil by performing compaction tests in a special mold as described in Annex A2. The five soil constants for Procedure B are determined in conjunction with compaction testing in accordance with specified compaction procedures, for example, Test Method D698 as described in Annex A3. Both Procedures A and B use Test Method D2216 to determine the water contents.
5.4 When following Procedure A, the water content is the average value over the length of the cylindrical mold and the density is the average value over the length of the multiple-rod probe embedded in the soil. When following Procedure B, the water content and density is the average values over the length of the multiple-rod embedded in the soil.
目前,国内外有很多种土壤水分测定方法,进而有不同的土壤水分传感器。比如:时域反射法(TDR),石膏法,红外遥感法,频域反射法/频域法(FDR/FD法),滴定法,电容法,电阻法,微波法,中子法,Karl Fischer法,γ射线法和核磁共振法等。 时域反射仪水分传感器 TDR法是上世纪80年代发展起来的一种土壤水分测定方法,中文为时域反射仪。...
土壤是人类赖以生存的自然资源之一,是植物生长发育的基础,土壤环境状态与人类社会的生存与繁衍息息相关。除水培植物之外,土壤水份是植物吸收水分的主要来源,土壤各类肥料的溶解和吸收,有机物的分解、转化也和土壤水分的含量有着紧密的关系。 土壤水分的衡量标准为土壤含水率,即水分重量占土壤重量的百分比。测定土壤含水量,掌握作物对水的需要情况,对农业生产有着重要的意义。...
它根据氢在急剧减低快中子的速度并把它们散射开的原则,现在市面上已经有测定土壤水分的中子水分计。中子水分计有很多方面的优点,但是对有机质土壤有相当的限制,而且它不适宜测定0-15cm的土壤水分含量。五、Y射线法水分传感器:与中子仪类似,射线透射法利用放射源137Cs放射出个线,用探头接收个射线透过土体后的能量,与土壤水分含量换算得到。...
目前,国内外有很多种土壤水分测定方法,进而有不同的土壤水分传感器。比如:时域反射法(TDR),石膏法,红外遥感法,频域反射法/频域法(FDR/FD法),滴定法,电容法,电阻法,微波法,中子法,Karl Fischer法,γ射线法和核磁共振法等。TDR法水分传感器:TDR法是上世纪80年代发展起来的一种土壤水分测定方法,中文为时域反射仪。...
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