infiltration index

精品项目网 2024-05-17 19:03:30

基本释义:

渗入指数

网络释义

1)infiltration index,渗入指数

2)infiltration index,入渗指数

3)infiltration experiential index,入渗经验指数

4)infiltration parameters,入渗参数

5)Kostiakov infiltration parameters,入渗参数

6)infiltration parameter,入渗参数

用法和例句

The surface stratum and the bottom of ploughed stratum of Yucheng experimental station being taken as investigated area,the steady infiltration rate fc and infiltration experiential index α are measured at about ninety-seven points.

以禹城综合试验站典型农田地块为研究对象,测得102 m×52 m面积内地表层与犁底层两个层面不同水平位置的土壤稳渗率f c与入渗经验指数α。

Spatial variability of the steady water infiltration rate and infiltration experiential index is studied with traditional statistics and Geo-statistics.

在中科院禹城综合试验站102 m×52 m面积内选择样点,采用经典统计学和地质统计学方法,对土壤稳渗率和入渗经验指数的空间变异性进行研究。

Improved Maheshiwari method for estimating infiltration parameters of soil;

估算土壤入渗参数的改进Mahesh wari法

Calculation and verification of infiltration parameters and roughness in furrow irrigation;

沟灌过程中土壤水分入渗参数与糙率的推求和验证

Experiment on vertical one-dimensional infiltration parameters under different head conditions;

蓄水坑灌条件下变水头作用的垂直一维土壤入渗参数试验研究

Optimized inverse model used to estimate Kostiakov infiltration parameters and Manning s roughness coefficient based on SGA and SRFR model:Ⅱ Application;

基于SGA和SRFR的畦灌入渗参数与糙率系数优化反演模型Ⅱ——模型应用

An optimized inverse model used to estimate Kostiakov infiltration parameters and Manning s roughness coefficient based on SGA and SRFR model:(Ⅰ) Establishment;

基于SGA和SRFR的畦灌入渗参数与糙率系数优化反演模型(Ⅰ)——模型建立

Linear regression approach for estimating soil infiltration parameters of border irrigation;

畦灌土壤入渗参数估算的线性回归法

Nonlinear regression method for estimating infiltration parameters according to border irrigation data;

用畦灌试验资料推求土壤入渗参数的非线性回归法

002 metric reflecting soil structure, effects of soil structure on infiltration capacity of field soils and three infiltration parameters of Kostiakov-Lewis infiltration equations were analyzed and discussed.

试验结果表明:土壤质地对大田土壤入渗能力的影响十分明显;土壤质地由轻变重,土壤入渗能力减小;3个入渗参数值随着土壤质地由轻变重而递减。

The Method Research of Infiltration Parameter Established by Routine Soil Physical Parameters;

用常规土壤物理参数确定入渗参数的方法研究

Infiltration capacity and parameters of freezing and thawing soil under different surface coverages

不同地表覆盖下冻融土壤入渗能力及入渗参数(英文)

Method Study on Determining Soil Infiltration Parameters with Pedo-Transfer Functions;

利用土壤传输函数确定入渗参数的方法研究

Estimation of infiltration parameters for border irrigation based on SIRMOD method and modelling of border irrigation

基于SIRMOD模型的畦灌入渗参数估算及灌溉模拟

Synchronously Determining Philip Infiltration Parameter and Synthesis Roughness Model of Border Irrigation

畦田Philip入渗参数和田面综合糙率同步推求

Optimal Inverse Method Applied for Determination of Soil Infiltration Parameter and Manning s Roughness Coefficient;

土壤入渗参数和糙率系数的优化反求方法及应用

Spatial Variability of Infiltration Parameters and Its Influences on Border Irrigation Performance

畦灌土壤入渗参数的空间变异性及其对灌水质量的影响

Determination of polymer flooding parameters for low permeable reservoirs

低渗透油层聚合物驱注入参数的确定

Calculation of hydraulic properties using the data measured by disc infiltrometers

用盘式负压入渗仪数据计算土壤导水参数

Groundwater recharge is an important parameter in hydrogeology.

地下水入渗补给量是重要的水文地质参数。

Research on the Spatial Variation of Soil Infiltration Characteristic Parameter;

区域尺度土壤入渗特征参数的变异性研究

Determination of Hydraulic Parameters of Stony-soil Media through Horizontal Infiltration

水平入渗法确定土石混合介质的水力参数分析

Influence of Water Supply Intensity on Infiltration Model Parameter under Non-sufficient Water Supply

供水强度对非充分供水入渗模型参数的影响

Study on Runoff and Infiltration Process and Hydraulic Parameters Characteristics with Grass Coverage

草被覆盖下坡面径流入渗过程及水力学参数特征试验研究

coefficient of recharge from irrigation

灌溉水入渗补给系数

A Study on Seepage Theory Model and Its Parameters in Rock Mass;

岩体渗流的理论模型及其渗流参数确定

NONLINEAR PARAMENTR IDENTIFICATION OF RELATIVE PERMEABILITY CHARACTERISTIC PARAMETER IN OIL AND GAS RESERVIOR

油气藏相渗特征参数的非线性参数识别

Analysis on Change Rule of the Precipitation Infiltration Compensating Coeffieient by Lysimeter

蒸渗计法降水入渗补给系数变化规律分析

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