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Ｂｏｄｍｏｄｓｓｔａｄｉｒ地热田是冰岛南部低温地热田之一．１９７４年以来，已完成１０口钻井．根据温度测井、井中压力和水位测量和一些地质地球物理资料研究，本文建立了它的概念模型．为了进一步建立该地热田的自然状态模型，本文进行了稳态和非稳态地温场模拟．通过假定一倾向北西的主断裂，模拟计算地温与观测地温吻合得很好．非稳态模拟还表明象这样的地热系统形成后５０００ａ就能达到准稳态（自然状态）．进一步通过求解质量和能量传输方程表明，该地热田深部补给在１０．０Ｌ／Ｓ，深部补给通道（断裂）的渗透率０．８达西．建立的自然状态模型能够用于这个地热田的评价和开发．
Bodmodsstadir geothermal field is one of the low-temperature geothermal fields in southern Iceland. Since 1974, 10 drilling wells have been completed. Based on temperature logging, well pressure and water level measurement and some geophysical and physical data research, this article establishes its conceptual model. In order to further establish the natural state model of the geothermal field, the steady-state and unsteady temperature field simulations were carried out. By assuming a dominant fault predominantly to the northwest, simulated ground temperature agrees well with observed ground temperature. Unsteady simulations also show that quasi-steady state (natural state) can be achieved in 5000 a geothermal systems like this. Further by solving the mass and energy transfer equations, it shows that the geothermal field has a deep recharge of 10.0 L / s and the deep recharge channel (fracture) has a permeability of 0.8 Darcy. The established natural state model can be used for the evaluation and development of this geothermal field.