Columnar joint morphology and cooling rate: A starch-water mixture experiment

被引:81
作者
Toramaru, A [1 ]
Matsumoto, T [1 ]
机构
[1] Kanazawa Univ, Dept Earth Sci, Kanazawa, Ishikawa 9201192, Japan
关键词
columnar joint; starch-water analogue experiment; cooling rate;
D O I
10.1029/2003JB002686
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
An analogue experiment using a starch-water mixture has been carried out in order to understand the effect of cooling rate on the morphological characteristics of a basalt columnar joint. If the contraction of material is essential for the formation of columnar joint structure, the water loss rate by desiccation (hereafter referred to as desiccation rate) in the experiment is analogous to the cooling rate in solidifying basalt. In the experiment the desiccation rate is controlled by varying the distance between the starch-water mixture and a lamp used as the heat source. We find that there are three regimes in the relation between joint formation and desiccation rate: (1) At desiccation rates higher than similar to1.4 x 10(-2) (g cm(-2) h(-1)) (normal columnar joint regime), the average cross-sectional area S of a column is inversely proportional to the average desiccation rate, [(M) over dot] (i.e., S proportional to [(M) over dot]-delta, with delta = 1). (2) Between that desiccation rate and a critical desiccation rate, 0.8 x 10(-2) (g/cm(2)h), S approaches infinity as [(M) over dot] <LF>decreases close to a critical desiccation rate (i.e., exponent delta monotonically increases from unity to infinity) (critical regime). (3) Below the critical desiccation rate, no columnar structure forms (no columnar joint regime forms). Applying the present experimental result to the formation of basalt column, the basalt columnar cross-sectional area is inversely proportional to the cooling rate with factors including elasticity, crack growth coefficient, thermal expansion, glass transition temperature, and crack density ratio at stress maximum. Also, it can be predicted that there exists a critical cooling rate below which the columnar joint does not form; the presence of a critical regime between the normal columnar jointing and no columnar jointing during a certain cooling rate range can also be predicted. We find that at higher cooling rate the preferred column shape is a pentagon, whereas at lower cooling rate it is a hexagon.
引用
收藏
页数:10
相关论文
共 29 条
[1]   EVOLUTION OF POLYGONAL FRACTURE PATTERNS IN LAVA FLOWS [J].
AYDIN, A ;
DEGRAFF, JM .
SCIENCE, 1988, 239 (4839) :471-476
[2]   MODELING THE EVOLUTION OF COLUMNAR JOINTS [J].
BUDKEWITSCH, P ;
ROBIN, PY .
JOURNAL OF VOLCANOLOGY AND GEOTHERMAL RESEARCH, 1994, 59 (03) :219-239
[3]   USE OF JOINT-GROWTH DIRECTIONS AND ROCK TEXTURES TO INFER THERMAL REGIMES DURING SOLIDIFICATION OF BASALTIC LAVA FLOWS [J].
DEGRAFF, JM ;
LONG, PE ;
AYDIN, A .
JOURNAL OF VOLCANOLOGY AND GEOTHERMAL RESEARCH, 1989, 38 (3-4) :309-324
[4]  
DEGRAFF JM, 1987, GEOL SOC AM BULL, V99, P605, DOI 10.1130/0016-7606(1987)99<605:SMOCJA>2.0.CO
[5]  
2
[6]   EFFECT OF THERMAL REGIME ON GROWTH INCREMENT AND SPACING OF CONTRACTION JOINTS IN BASALTIC LAVA [J].
DEGRAFF, JM ;
AYDIN, A .
JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH, 1993, 98 (B4) :6411-6430
[7]   Conductive cooling of lava: Columnar joint diameter and stria width as functions of cooling rate and thermal gradient [J].
Grossenbacher, KA ;
McDuffie, SM .
JOURNAL OF VOLCANOLOGY AND GEOTHERMAL RESEARCH, 1995, 69 (1-2) :95-103
[8]   Patterns and scaling in surface fragmentation processes [J].
Hornig, T ;
Sokolov, IM ;
Blumen, A .
PHYSICAL REVIEW E, 1996, 54 (04) :4293-4298
[9]   THE GROWTH OF GRAIN-BOUNDARY VOIDS UNDER STRESS [J].
HULL, D ;
RIMMER, DE .
PHILOSOPHICAL MAGAZINE, 1959, 4 (42) :673-687
[10]  
Jones F.E., 1992, Evaporation of water: with emphasis on applications and measurements