๐”– Bobbio Scriptorium
โœฆ   LIBER   โœฆ

Biogeochemical and hydrological controls on carbon export from a forested catchment in central Japan

โœ Scribed by Masatoshi Kawasaki; Nobuhito Ohte; Masanori Katsuyama


Publisher
Springer
Year
2005
Tongue
English
Weight
634 KB
Volume
20
Category
Article
ISSN
0912-3814

No coin nor oath required. For personal study only.


๐Ÿ“œ SIMILAR VOLUMES


Hydrological versus biogeochemical contr
โœ Carlos J. Ocampo; Carolyn E. Oldham; Murugesu Sivapalan; Jeffrey V. Turner ๐Ÿ“‚ Article ๐Ÿ“… 2006 ๐Ÿ› John Wiley and Sons ๐ŸŒ English โš– 690 KB

Deciphering the connection between streamflows and nitrate (NO 3 ) discharge requires identification of the various water flow pathways within a catchment, and the different time-scales at which hydrological and biogeochemical processes occur. Despite the complexity of the processes involved, many c

Hydrological control of dissolved organi
โœ Masatoshi Kawasaki; Nobuhito Ohte; Naoki Kabeya; Masanori Katsuyama ๐Ÿ“‚ Article ๐Ÿ“… 2008 ๐Ÿ› John Wiley and Sons ๐ŸŒ English โš– 628 KB

## Abstract To evaluate the influence of hydrological processes on dissolved organic carbon (DOC) dynamics in a forested headwater catchment, DOC concentration was observed along the flow path from rainfall to stream water via throughfall, soil water, groundwater, and spring water for 4 years, and

Impact of climate change on runoff from
โœ Yoshinori Shinohara; Tomo'omi Kumagai; Kyoichi Otsuki; Atsushi Kume; Naoya Wada ๐Ÿ“‚ Article ๐Ÿ“… 2009 ๐Ÿ› John Wiley and Sons ๐ŸŒ English โš– 282 KB ๐Ÿ‘ 1 views

## Abstract Hydrologic balance in highโ€altitude, midโ€latitude mountain areas is important in terms of the water resources available to associated lowlands. This study examined how current and historical shifts in precipitation (__P__) patterns and concurrent increases in temperature (__T__) affecte

Soil partitioning and surface store cont
โœ R. A. Metcalfe; J. M. Buttle ๐Ÿ“‚ Article ๐Ÿ“… 2001 ๐Ÿ› John Wiley and Sons ๐ŸŒ English โš– 494 KB

## Abstract The midโ€ to highโ€boreal forest in Canada occupies the discontinuous permafrost zone, and is often underlain by glaciolacustrine sediments mantled by a highly porous organic mat. The result is a poorly drained landscape dominated by wetlands. Frostโ€table dynamics and surface storage cond