共找到 145 条与 土壤的水文特性 相关的标准,共 10 页
This Standard specifies laboratory methods for determination of the soil water-retention characteristics. This Standard applies only to measurements of the drying or desorption curve. Four methods are described to cover the complete range of soil water pressures. Guidelines are given to select the most suitable method in a particular case.
Soil quality - Determination of the water-retention characteristics - Laboratory methods
This International Standard specifies laboratory methods for determination of the soil water-retention characteristic. This International Standard applies only to measurements of the drying or desorption curve. Four methods are described to cover the complete range of soil water pressures as follows: a) method using sand, kaolin or ceramic suction tables for determination of matric pressures from 0 kPa to -50 kPa; b) method using a porous plate and burette apparatus for determination of matric pressures from 0 kPa to - 20 kPa; c) method using a pressurized gas and a pressure plate extractor for determination of matric pressures from -5kPa to-1500kPa; d) method using a pressurized gas and pressure membrane cells for determination of matric pressures from -33kPa to-1500kPa. Guidelines are given to select the most suitable method in a particular case.
Soil quality - Physical methods - Laboratory methods
Soil quality. Determination of the water retention characteristic. Laboratory methods
Soil quality. Determination of the water-retention characteristic. Laboratory methods
This International Standard describes three methods for the determination of dry bulk density of soils calculated from the mass and the volume of a soil sample. The methods involve drying and weighing a soil sample, the volume of which is either known (core method, see 4.1) or has to be determined (excavation method, see 4.2, and clod method, see 4.3).
Soil quality - Physical methods - Determination of dry bulk density
Soil quality. Determination of dry bulk density.
Soil quality - Determination of the water-retention characteristic - Laboratory methods.
This International Standard specifies laboratory methods for determination of the soil water-retention characteristic. This International Standard applies only to measurements of the drying or desorption curve. Four methods are described to cover the complete range of soil water pressures as follows: a) method using sand, kaolin or ceramic suction tables for determination of matric pressures from 0 kPa to -50 kPa; b) method using a porous plate and burette apparatus for determination of matric pressures from 0 kPa to -20 kPa; c) method using a pressurized gas and a pressure plate extractor for determination of matric pressures from -5kPa to -1500kPa; d) method using a pressurized gas and pressure membrane cells for determination of matric pressures from -33kPa to -1500kPa. Guidelines are given to select the most suitable method in a particular case.
Soil quality - Determination of the water-retention characteristic - Laboratory methods
This International Standard describes three methods for the determination of dry bulk density of soils calculated from the mass and the volume of a soil sample. The methods involve drying and weighing a soil sample, the volume of which is either known (core method, see 4.1) or has to be determined (excavation method, see 4.2, and clod method, see 4.3).
Soil quality - Determination of dry bulk density
This International Standard specifies methods for the determination of pore water pressure in both unsaturated and saturated soil using tensiometers.
Soil quality - Determination of pore water pressure - Tensiometer method
This International Standard specifies an in situ method for the determination of water content in the unsaturated zone of soils using a neutron depth probe.
Soil quality - Determination of water content in the unsaturated zone - Neutron depth probe method
The document specifies a method for the determination of the dry matter content and water content of soil samples on a mass basis. This method can be applied to all types of soil samples. Different procedures are specified for air-dried soil samples (samples pretreated and field-moist soil samples). For the determination of soil water content on a volume basis refer to ISO 11461.
Soil quality - Determination of dry matter and water content on a mass basis - Gravimetric method (ISO 11465:1993)
Non-destructive method suitable for repeated measurements.
Soil quality. Physical methods. Determination of water content in the unsaturated zone. Neutron depth probe method
Soil quality. Determination of water content of the unsaturated zone. Neutron depth probe method.
Applicable to both saturated and unsaturated soils.
Soil quality - Physical methods - Determination of pore water pressure - Tensiometer method
Specifies a non-destructive method for the determination of water content in the unsaturated zone of soils using a neutron depth probe. Water content profiles can be obtained by measuring at a series of depths of soil.
Soil-quality - Determination of water content in the unsaturated zone - Neutron depth probe method
Soil quality. Determination of pore water pressure. Tensiometer method.
Describes methods for the determination of pore water pressure (point measurements) in unsaturated and saturated soil using tensiometers. Applicable for in situ measurements in the field and, e. g. soil cores, used in experimental examinations.
Soil quality - Determination of pore water pressure - Tensiometer method
Qualité des sols - Méthode de mesurage de la conductivité hydraulique horizontale équivalente et de la porosité de drainage in situ - Méthode de Guyon.
1.1 This test method covers the determination of elastic moduli of intact rock core specimens in undrained triaxial compression. It specifies the apparatus, instrumentation, and procedures for determining the stress-axial strain and the stress-lateral strain curves, as well as Young''s modulus, E, and Poisson''s ratio, v. Note 1--This test method does not include the procedures necessary to obtain a stress-strain curve beyond the ultimate strength.1.2 For an isotropic material, the relation between the shear and bulk moduli and Young''s modulus and Poisson''s ratio are: Equation 1 - G = E/2(1 + v) Equation 2 - K = E/3(1 - 2v)where: G = shear modulus,K = bulk modulus, E = Young''s modulus, andv = Poisson''s ratio. 1.2.1 The engineering applicability of these equations is decreased if the rock is anisotropic. When possible, it is desirable to conduct tests in the plane of foliation, bedding, etc., and at right angles to it to determine the degree of anisotropy. It is noted that equations developed for isotropic materials may give only approximate calculated results if the difference in elastic moduli in any two directions is greater than 10 % for a given stress level.Note 2--Elastic moduli measured by sonic methods may often be employed as preliminary measures of anisotropy.1.3 This test method given for determining the elastic constants does not apply to rocks that undergo significant inelastic strains during the test, such as potash and salt. The elastic moduli for such rocks should be determined from unload-reload cycles, that is not covered by this test method.1.4 The values stated in SI units are to be regarded as the standard.1.5 This standard does not purport to address all of the safety concerns, if any, associated with its use. It is the responsibility of the user of this standard to establish appropriate safety and health practices and determine the applicability of regulatory limitations prior to use. Specific safety precautions are given in Section 6.
Standard Test Method for Elastic Moduli of Undrained Intact Rock Core Specimens in Triaxial Compression Without Pore Pressure Measurement
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