煤田地质与勘探
煤田地質與勘探
매전지질여감탐
COAL GEOLOGY & EXPLORATION
2015年
4期
102-105
,共4页
构造煤%阻抗振幅%水分%优势频段
構造煤%阻抗振幅%水分%優勢頻段
구조매%조항진폭%수분%우세빈단
tectonic coal%impedance amplitude%moisture%edge band
通过测定不同地点的6种不同变质程度的构造煤在常温常压下的阻抗振幅,得到不同类型构造煤振幅谱各自不同的特点,在所测100 Hz~100 kHz 频率范围内,各类构造煤 Z–f(阻抗振幅–频率)呈一条单调递减曲线。在交变电场下烟煤的导电性较无烟煤及其他岩石差。在所测频段内,无烟煤 Z 值明显低于烟煤,且差值随着 f 增大逐渐减小。通过对构造煤 Z–M(阻抗振幅–水分)的拟合,得到相关公式;再利用所得构造煤阻抗振幅验证其公式可靠性,找出优势频段。初步分析了煤岩的幅频特性,为试图利用煤岩电性频率域响应特征差异来反映不同变质程度构造煤及与其他岩矿石的导电机理及结构模型,进而为用电法勘探物质组成与结构提供理论与实验基础。
通過測定不同地點的6種不同變質程度的構造煤在常溫常壓下的阻抗振幅,得到不同類型構造煤振幅譜各自不同的特點,在所測100 Hz~100 kHz 頻率範圍內,各類構造煤 Z–f(阻抗振幅–頻率)呈一條單調遞減麯線。在交變電場下煙煤的導電性較無煙煤及其他巖石差。在所測頻段內,無煙煤 Z 值明顯低于煙煤,且差值隨著 f 增大逐漸減小。通過對構造煤 Z–M(阻抗振幅–水分)的擬閤,得到相關公式;再利用所得構造煤阻抗振幅驗證其公式可靠性,找齣優勢頻段。初步分析瞭煤巖的幅頻特性,為試圖利用煤巖電性頻率域響應特徵差異來反映不同變質程度構造煤及與其他巖礦石的導電機理及結構模型,進而為用電法勘探物質組成與結構提供理論與實驗基礎。
통과측정불동지점적6충불동변질정도적구조매재상온상압하적조항진폭,득도불동류형구조매진폭보각자불동적특점,재소측100 Hz~100 kHz 빈솔범위내,각류구조매 Z–f(조항진폭–빈솔)정일조단조체감곡선。재교변전장하연매적도전성교무연매급기타암석차。재소측빈단내,무연매 Z 치명현저우연매,차차치수착 f 증대축점감소。통과대구조매 Z–M(조항진폭–수분)적의합,득도상관공식;재이용소득구조매조항진폭험증기공식가고성,조출우세빈단。초보분석료매암적폭빈특성,위시도이용매암전성빈솔역향응특정차이래반영불동변질정도구조매급여기타암광석적도전궤리급결구모형,진이위용전법감탐물질조성여결구제공이론여실험기출。
Impedance amplitude measurement of six metamorphic kinds of tectonic coal was conducted under normal pressure and temperature. And then some phenomena were concluded as follows: amplitude spectrum of coal of different kinds respectively present different characteristics. In the test frequency range of 100 Hz~100 kHz, Z-f curves of coals all show monotone decrease. Through fitting of Z-M of tectonic coal, we can draw relevant formula, and use coal to validate, as the result, the edge band is obtained. In order to try to use coal and rock elec-trical response characteristic differences in frequency domain to reflect different conductive mechanisms and structure models of different coals and rocks, and then to use electricity exploration to prospect its compositions and structures, theoretical and experimental basis have been provided.