HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS		QUICK SEARCH:   [advanced] Author: Keyword(s): Year:  Vol:  Page:

This Article Figures Only Full Text Full Text (PDF) Alert me when this article is cited Alert me if a correction is posted Services Similar articles in this journal Alert me to new issues of the journal Download to citation manager Google Scholar Articles by Katsura, S. Articles by Mizuyama, T. PubMed Articles by Katsura, S. Articles by Mizuyama, T. GeoRef GeoRef Citation Agricola Articles by Katsura, S. Articles by Mizuyama, T. Related Collections Hydraulic Conductivity Water Retention/Capillary Pressure Downhole/Borehole Methods

ORIGINAL RESEARCH

Hydraulic Properties of Variously Weathered Granitic Bedrock in Headwater Catchments

Dep. of Forest Science, Graduate School of Agriculture, Kyoto Univ., Kyoto, Japan
^* Corresponding author (katsura3{at}kais.kyoto-u.ac.jp).

Received 5 October 2008.

Recent studies have emphasized the importance of bedrock in hydrologic processes occurring in headwater catchments. To understand water flow processes through variously weathered bedrock, we measured the saturated hydraulic conductivity, K_s, and water retention characteristics of weakly to highly weathered Tanakami granite and Rokko granite core samples. On the basis of these core-scale properties, along with the core shape and in situ K_s measurements, we defined two groups of bedrock: C_M class (weakly weathered) and C_L to D_L class (moderately to highly weathered). The C_M class bedrock cores had almost no effective porosity (i.e., the amount of porosity that effectively contributes to water flow) and therefore extremely small core-scale K_s, indicating that the matrix could be regarded as essentially impermeable. The in situ K_s was much larger than the core-scale values, however, and the core shape showed apparent fractures, suggesting that water did flow preferentially through the fractures. The volumetric water content of the C_L– to D_L–class bedrock water retention curves changed little in the dry range but changed gradually in the wet range, resulting in a moderate core-scale K_s of 10^–5 to 10^–3 cm s^–1. The core-scale K_s values were well explained by the parameters characterizing the water retention curve. The similarity of the in situ K_s to the core-scale values, and the lack of fractures in the core shape, suggested that water flow could be characterized as matrix flow. The hydraulic properties of weathered granite at other sites followed the trends observed at our sites, implying wide applicability of the findings in this study to various types of weathered granite.

Abbreviations: KEW, Kiryu Experimental Watershed • NEW, Nishi'otafuku-Yama Experimental Watershed • WRC, water retention characteristic