作者: 假設(shè) 時(shí)間: 2025-3-21 22:27 作者: Default 時(shí)間: 2025-3-22 01:29
Soil-Water Content and Its Measurement,e varieties of methods with continuous output are briefly described; neutron method, capacitance method, electrical resistance method, time-domain reflectometry (TDR), frequency-domain reflectometry (FDR), and geophysical and remote-sensing methods.作者: Throttle 時(shí)間: 2025-3-22 07:18 作者: 參考書目 時(shí)間: 2025-3-22 10:57 作者: 混雜人 時(shí)間: 2025-3-22 13:57
https://doi.org/10.1007/1-4020-3776-7valuation from measured data. Analytical expressions of the SWRC are presented and evaluations of useful “hydrolimits” like monomolecular water capacity, wilting point, available water capacity and field capacity using SWRC data are described.作者: 使習(xí)慣于 時(shí)間: 2025-3-22 17:33
https://doi.org/10.1007/1-4020-3776-7he influences of the rain rate, entrapped air, initial soil-water content and layered soil profile on infiltration dynamics are discussed. Methods for the estimation of the soil hydraulic conductivity using the infiltration process in the field are described as well.作者: ETHER 時(shí)間: 2025-3-22 23:55
The Input Side of the Material Flow Balance, together with the continuity equation to derive the convective–diffusion transport equation. The Péclet number is used to evaluate the transport mechanisms of dissolved compounds. Outflow and breakthrough curves are defined, described and explained to identify the character and significance of the solute transport.作者: gene-therapy 時(shí)間: 2025-3-23 03:54
How To Organize An Ema Pilot Project,t can be proposed and an expected yield can be calculated. Based on analysis of soil-water balance equations, one can propose the principles of soil-water management. Hydrological classification of the soil-water regimen and the principles of soil-water regimen diagnostics are presented.作者: Aphorism 時(shí)間: 2025-3-23 08:06 作者: 懸崖 時(shí)間: 2025-3-23 09:54
Soil-Water Retention Curve,valuation from measured data. Analytical expressions of the SWRC are presented and evaluations of useful “hydrolimits” like monomolecular water capacity, wilting point, available water capacity and field capacity using SWRC data are described.作者: 緯線 時(shí)間: 2025-3-23 14:51
Infiltration of Water into Soil,he influences of the rain rate, entrapped air, initial soil-water content and layered soil profile on infiltration dynamics are discussed. Methods for the estimation of the soil hydraulic conductivity using the infiltration process in the field are described as well.作者: Collision 時(shí)間: 2025-3-23 19:56 作者: corporate 時(shí)間: 2025-3-23 22:43
Water and Energy Balance in the Field and Soil-Water Regimen,t can be proposed and an expected yield can be calculated. Based on analysis of soil-water balance equations, one can propose the principles of soil-water management. Hydrological classification of the soil-water regimen and the principles of soil-water regimen diagnostics are presented.作者: 充氣女 時(shí)間: 2025-3-24 02:26
Book 2019 the estimation and application of measurements and evaluation of soil-hydrophysical characteristics using simulation models, with a focus on elucidating the basic hydrophysical characteristics of soil, such as soil water potential and hydraulic conductivity, as well as the methods of measurement. I作者: APNEA 時(shí)間: 2025-3-24 09:09 作者: 生意行為 時(shí)間: 2025-3-24 14:21 作者: GIST 時(shí)間: 2025-3-24 16:02 作者: 連系 時(shí)間: 2025-3-24 22:19 作者: 駁船 時(shí)間: 2025-3-24 23:35 作者: Yag-Capsulotomy 時(shí)間: 2025-3-25 05:35 作者: transient-pain 時(shí)間: 2025-3-25 11:18 作者: nauseate 時(shí)間: 2025-3-25 13:19 作者: Pelvic-Floor 時(shí)間: 2025-3-25 18:53 作者: Stress-Fracture 時(shí)間: 2025-3-25 20:25
Eco-Efficiency in Industry and Sciencellency: contact angle, severity of water repellency, persistence of soil water repellency and index of water repellency. It also presents the hydrophobic compounds in soils and the influence of soil-water repellency on hydrological processes in soil (infiltration, preferential flow, evaporation).作者: 行乞 時(shí)間: 2025-3-26 03:12
,Soil as a Part of the Soil–Plant–Atmosphere Continuum (SPAC),sed. Soil water is always a low concentrated solution, but its physical properties are not changed significantly, and therefore it can be assumed to be clean water. The solute concentration is considered to evaluate the increased risk of soil salinization. The role of carbon dioxide in the SPAC system and its role in climate change are discussed.作者: 雪崩 時(shí)間: 2025-3-26 05:45
Basic Physical Characteristics of Soils, of various soil types are described, as well as their role in the formation of soil physical properties. The influence of clay minerals in soil physical properties formation and mechanisms of their interaction with soil water are demonstrated.作者: Water-Brash 時(shí)間: 2025-3-26 11:53 作者: commute 時(shí)間: 2025-3-26 14:11
Soil-Water Movement in Water-Saturated Capillary Porous Media, the measurement of saturated hydraulic conductivity above the groundwater table are presented and discussed. Pedotransfer functions to evaluate hydraulic conductivity from available data are briefly discussed.作者: Feigned 時(shí)間: 2025-3-26 20:11 作者: 污穢 時(shí)間: 2025-3-26 23:54 作者: 珊瑚 時(shí)間: 2025-3-27 01:52 作者: 匍匐 時(shí)間: 2025-3-27 08:37
Swelling and Shrinking Soils,ration into dry, heavy soils; they significantly increase the retention volume of such soils and the infiltration surface of water-filling soil cracks. The importance of water infiltration into the soil matrix from cracks surface is demonstrated.作者: Autobiography 時(shí)間: 2025-3-27 09:32
Water Repellent Soils,llency: contact angle, severity of water repellency, persistence of soil water repellency and index of water repellency. It also presents the hydrophobic compounds in soils and the influence of soil-water repellency on hydrological processes in soil (infiltration, preferential flow, evaporation).作者: Arb853 時(shí)間: 2025-3-27 16:26 作者: 索賠 時(shí)間: 2025-3-27 19:18
Redistribution of Water in Homogeneous Soil,ary/initial conditions on the rate of redistribution. The quantification of the redistribution process by the solution of the Richards equation assuming constant hydraulic conductivity of soil demonstrates the logarithmic decrease of soil-water movement during redistribution, thus preserving soil water for plants.作者: Abrade 時(shí)間: 2025-3-27 23:18
Stony Soils,o contains links to the latest literature in this area. An illustrative example of the evaluation of effective stony-soil parameters for particular stony soil from the Western High Tatra Mts. (Slovakia) and results of the illustrative water-flow modelling in the stony soil (a case study) are presented and discussed.作者: 致敬 時(shí)間: 2025-3-28 03:17
Soil Air and Its Dynamics,ith an atmosphere. This chapter analyses the convection and diffusion of air in the soil and expresses them quantitatively. It also quantifies oxygen transport to the plant roots to cover respiration by solving the simplified transport equation. The influence of the oxygen diffusion rate on plant canopy growth is also presented.作者: obnoxious 時(shí)間: 2025-3-28 10:07 作者: 豐富 時(shí)間: 2025-3-28 10:51
https://doi.org/10.1007/1-4020-3776-7ary/initial conditions on the rate of redistribution. The quantification of the redistribution process by the solution of the Richards equation assuming constant hydraulic conductivity of soil demonstrates the logarithmic decrease of soil-water movement during redistribution, thus preserving soil water for plants.作者: 浮夸 時(shí)間: 2025-3-28 15:08 作者: etiquette 時(shí)間: 2025-3-28 21:45
Eco-Efficiency in Industry and Scienceith an atmosphere. This chapter analyses the convection and diffusion of air in the soil and expresses them quantitatively. It also quantifies oxygen transport to the plant roots to cover respiration by solving the simplified transport equation. The influence of the oxygen diffusion rate on plant canopy growth is also presented.作者: Daily-Value 時(shí)間: 2025-3-29 01:13 作者: 調(diào)整 時(shí)間: 2025-3-29 04:05
978-3-030-13195-1Springer Nature Switzerland AG 2019作者: nostrum 時(shí)間: 2025-3-29 11:10
Applied Soil Hydrology978-3-030-01806-1Series ISSN 0924-6118 Series E-ISSN 2213-6940 作者: 縫紉 時(shí)間: 2025-3-29 13:17
Viliam Novák,Hana Hlavá?ikováPresents basic topics of soil hydrology clearly, making it suitable for a wide range of researchers and students.Extremely well illustrated and complemented with practical tables.Explores specific top作者: 男生戴手銬 時(shí)間: 2025-3-29 18:44
Theory and Applications of Transport in Porous Mediahttp://image.papertrans.cn/b/image/160141.jpg作者: 歌唱隊(duì) 時(shí)間: 2025-3-29 20:11
https://doi.org/10.1007/1-4020-3776-7in the case of bare soil or the water table, the SPAC system is reduced to the Soil–Atmosphere Continuum (SAC) or to the Water-Table–Atmosphere Continuum (WAC). This chapter contains basic information about all three subsystems of SPAC. Conceptual approaches to the soil-water and energy transport ar作者: mercenary 時(shí)間: 2025-3-30 00:17
https://doi.org/10.1007/1-4020-3776-7s a three-phase system, composed of solid, liquid and gaseous components, the basic properties of all three phases are described and quantified. Definitions of soil porosity, specific bulk density, bulk density, aeration, soil water content and soil specific surface are presented. Soil texture is de作者: indices 時(shí)間: 2025-3-30 07:45
https://doi.org/10.1007/1-4020-3776-7imultaneously in all three phases: ice, liquid water and water vapour. Its dynamics are linked to the great expenditure of energy to keep in motion ‘the water cycle and thus stabilize Earth’s climatic conditions. Water’s occurrence and its movement are preconditions for biomass production. In this c作者: Rustproof 時(shí)間: 2025-3-30 08:13 作者: Crepitus 時(shí)間: 2025-3-30 15:06 作者: 無(wú)法解釋 時(shí)間: 2025-3-30 20:09 作者: Accommodation 時(shí)間: 2025-3-30 21:29 作者: 漸強(qiáng) 時(shí)間: 2025-3-31 01:20
https://doi.org/10.1007/1-4020-3776-7o water flow and water-potential distribution for various configurations of soil samples is described. The Darcian approach to saturated soil-water movement assumes the porous space is fully saturated with water; the soil pores do not change their dimensions, and soil temperature is constant. Hydrau作者: Acumen 時(shí)間: 2025-3-31 08:35 作者: Blatant 時(shí)間: 2025-3-31 12:25 作者: 搖晃 時(shí)間: 2025-3-31 13:43 作者: FIN 時(shí)間: 2025-3-31 17:53
https://doi.org/10.1007/1-4020-3776-7water can significantly improve the supply to plants of water and nutrients. A groundwater depth of about two metres below the soil surface is assumed to be the critical depth that contributes markedly to the supply of water to the plant canopy. In this chapter, the vertical transport of water from 作者: 的染料 時(shí)間: 2025-3-31 22:54
Springer Tracts in Civil Engineeringthods for evapotranspiration estimation, as well as the calculation methods to estimate its structural components: evaporation and transpiration. The basic equations of potential evapotranspiration calculation (the Penman equation) and actual evapotranspiration calculation (the Penman–Monteith equat作者: 愛國(guó)者 時(shí)間: 2025-4-1 03:26
