【摘要】 对海阳湾外侧浅水区域实测水体运动特征及其对应的沉积磁组构参量 ,采用线性回归方法进行统计分析 ,取得的结果是 :EV1 (估算流速 1) =17.372 4- 2 .16 87(P- 1.0 )× 10 0 +10 .890 9(Fs- 1.0 )× 10 0 ,其估计平均误差 (V(实测流速 ) - EV1 ) =0 .2 83;EV2 (估算流速 2 ) =- 886 .1178- 2 87.6 32 1P+1191.1870 Fs,其估计平均误差 (V- EV2 ) =0 .2 98。初步探讨结果表明 ,水体运移小潮期最大涨潮流底层流流速与沉积磁组构参量 P、Fs对应关系研究是可行的。更多还原

【Abstract】 In this paper we discussed characteristics of observed bottom currents and corresponding magnetic fabric parameters of sediments in the shallow water out of Haiyang Bay and did statistical analyses by making use of regression method.The analysis results are: EV 1 (estimated current velocity 1)=17 372 4-2 168 7( P-1 0)×100+10 890 9(F s-1 0)×100,estimated average error[ V (observed current velocity) EV 1]=0 283;EV 2 (estimated current velocity 2)=-886 117 8-287 632 1 P+1 191.187 0F s,and estimated average error( V-EV 2)=0 298. The preliminary results also indicated that there were corresponding relations between the maximum flood bottom current velocity in neap season and magnetic fabric parameters P and F s.The results are extensively used in paleoceanographical and paleolimnological researches in order to solve problems that are unsolved now.更多还原