نتایج جستجو برای: hydraulic gradient

تعداد نتایج: 154232  

2010
A. C. FOWLER

Of several problems associated with theoretical explanations of the jokul­ hlaups which emerge from the outlet glacier Skeioararj okull of the ice c ap Vatnajokull i n southeast Iceland, the mechanism of flood ini ti atio n i s one that has h itherto defied explanation. We provide such an explanation based on a careful analysis of the classical Nye-Rothlisberger model; near the subglacial lake ...

2011
Raj Mohan Singh

Most of the hydraulic structures are founded on permeable foundation. There is, however, no procedure to fix the basic barrage parameters, which are depth of sheet piles/cutoffs and the length and thickness of floor, in a cost-effective manner. Changes in hydrological and climatic factors may alter the design seepage head of the hydraulic structures. The variation in seepage head affects the do...

Journal: :Plant, cell & environment 2006
R N Addington L A Donovan R J Mitchell J M Vose S D Pecot S B Jack U G Hacke J S Sperry R Oren

We investigated relationships between whole-tree hydraulic architecture and stomatal conductance in Pinus palustris Mill. (longleaf pine) across habitats that differed in soil properties and habitat structure. Trees occupying a xeric habitat (characterized by sandy, well-drained soils, higher nitrogen availability and lower overstory tree density) were shorter in stature and had lower sapwood-t...

2007
P. Kumar G. G. Amenu

Introduction Conclusions References Tables Figures ◭ ◮ ◭ ◮ Back Close Full Screen / Esc Papers published in Hydrology and Earth System Sciences Discussions are under open-access review for the journal Hydrology and Earth System Sciences Abstract Introduction Conclusions References Tables Figures ◭ ◮ ◭ ◮ Back Close Full Screen / Esc Abstract One of the adaptive strategies of vegetation, particul...

2006
Alan REMPEL

Glaciers are permeated by liquid veins that line the triple junctions between ice grains and act as conduits for material transport. The density difference between water and ice produces a hydraulic gradient that drives liquid flow down towards the glacier bed. We investigate how variations in this transport rate are manifest in the lower regions of a glacier that floats on a subglacial reservo...

2013
Erhan Caliskan

Forest roads are the base infrastructure foundation of forestry operations. These roads entail a complex engineering effort because they can cause substantial environmental damage to forests and include a high-cost construction. This study was carried out in four sample sites of Giresun, Trabzon(2) and Artvin Forest Directorate, which is in the Black Sea region of Turkey. The areas have both st...

2016
Usman Anwar Randall K. Kolka John Tyndall Randall Kolka

Predicting the hydrologic consequences of biomass cropping systems requires an understanding of how different crops and management practices affect soil hydraulic properties across space and time. To inform such predictions, I investigated the impacts of five biomass cropping systems on the hydraulic properties of soils across a landscape gradient in wet, dry, and average rainfall years. I used...

2008
Jennifer E. Pyzoha Timothy J. Callahan Ge Sun Carl C. Trettin Masato Miwa

This paper describes how climate influences the hydrology of an ephemeral depressional wetland. Surface water and groundwater elevation data were collected for 7 years in a Coastal Plain watershed in South Carolina USA containing depressional wetlands, known as Carolina bays. Rainfall and temperature data were compared with water-table well and piezometer data in and around one wetland. Using t...

Journal: :Plant physiology 2016
Hugo J de Boer Paul L Drake Erin Wendt Charles A Price Ernst-Detlef Schulze Neil C Turner Dean Nicolle Erik J Veneklaas

Leaf veins supply the mesophyll with water that evaporates when stomata are open to allow CO2 uptake for photosynthesis. Theoretical analyses suggest that water is optimally distributed in the mesophyll when the lateral distance between veins (dx) is equal to the distance from these veins to the epidermis (dy), expressed as dx:dy ≈ 1. Although this theory is supported by observations of many de...

Journal: :Plant physiology 1983
D J Cosgrove R E Cleland

The water transport properties of etiolated pea (Pisum sativum L.) internodes were studied using both dynamic and steady-state methods to determine (a) whether water transport through the growing tissue limits the rate of cell enlargement, and (b) whether auxin stimulates growth in part by increasing the hydraulic conductance of the growing tissue.Measurements using the pressure probe technique...

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