Knowledge

Thaw depth

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153:
Oelke, C., T. Zhang, M. Serreze, and R. Armstrong, 2003: Regional-scale modeling of soil freeze/thaw over the Arctic drainage basin. J. Geophys. Res., 108 (D10): Art.No. 4314 May 29, 2003.
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is the instantaneous level down to which the soil has warmed to zero degrees Celsius. The active layer thickness is the maximum thaw depth over a period of two years.
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In construction, the thaw depth is a major factor in ensuring the structural integrity of the objects in question.
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cannot penetrate beyond the active layer, which places restrictions on which plants can grow in permafrost.
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The knowledge of the thaw depth is important for the two major reasons: its influence on the
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refers to the varying position of the thaw line during the periods of freezing/thawing.
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The primary factor that determines the thaw depth is the maximal air temperature. The
115: 82: 138:, which influence the bulk density of the soil, and hence thermal conductivity. 162: 78: 111: 54: 32: 17: 131: 36: 69:, etc.). These influences are mediated by the effects of the dynamics 107: 86: 58: 70: 50: 97: 127: 123: 93: 66: 31:
The layer of soil over the thaw depth is called the
160: 126:soils have much deeper thaw line than 161: 110:is another important factor: coarser 13: 14: 195: 35:, while the soil below is called 147: 1: 141: 7: 10: 200: 134:and the percentage of the 89:processes in permafrost. 130:. Other factors are the 120:thermal conductivity 136:soil organic matter 191: 154: 151: 199: 198: 194: 193: 192: 190: 189: 188: 179:Ground freezing 159: 158: 157: 152: 148: 144: 116:parent material 12: 11: 5: 197: 187: 186: 181: 176: 171: 156: 155: 145: 143: 140: 122:, and, e.g., 83:biogeochemical 79:geomorphologic 9: 6: 4: 3: 2: 196: 185: 182: 180: 177: 175: 172: 170: 167: 166: 164: 150: 146: 139: 137: 133: 129: 125: 121: 117: 113: 109: 104: 101: 99: 95: 92:In ecology, 90: 88: 84: 80: 76: 72: 68: 64: 60: 56: 52: 47: 45: 40: 38: 34: 29: 27: 23: 19: 169:Soil science 149: 118:have higher 105: 102: 91: 55:construction 48: 43: 41: 33:active layer 30: 25: 21: 18:soil science 15: 44:frost front 184:Permafrost 174:Glaciology 163:Categories 142:References 132:vegetation 87:hydrologic 71:biological 37:permafrost 22:thaw depth 108:soil type 75:pedologic 63:pipelines 59:buildings 42:The term 26:thaw line 112:textures 114:of the 53:and on 51:ecology 98:plants 85:, and 20:, the 128:clays 124:sandy 94:roots 67:roads 96:of 24:or 16:In 165:: 81:, 77:, 73:, 65:, 61:, 39:. 57:(

Index

soil science
active layer
permafrost
ecology
construction
buildings
pipelines
roads
biological
pedologic
geomorphologic
biogeochemical
hydrologic
roots
plants
soil type
textures
parent material
thermal conductivity
sandy
clays
vegetation
soil organic matter
Categories
Soil science
Glaciology
Ground freezing
Permafrost

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