TURBIDITY MAXIMUM OF NORTHERN CHESAPEAKE BAY

被引:181
作者
SCHUBEL, JR
机构
[1] Chesapeake Bay Institute, Johns Hopkins University, Baltimore
关键词
D O I
10.1126/science.161.3845.1013
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 ; 0710 ; 09 ;
摘要
The turbidity maximum near the head of the Chesapeake Bay is produced primarily by the local resuspension of bottom sediments, and by the estuarine sediment trap" which is formed in the upper reaches of the estuarine circulation regime by the net nontidal circulation."
引用
收藏
页码:1013 / &
相关论文
共 9 条
  • [1] Glangeaud L., 1938, B SOC GEOL FR, V8, P599
  • [2] IPPEN AT, 1966, ESTUARY COASTLINE HY, P648
  • [3] LUNEBURG H, 1939, ARCH DEUT SEEWARTE, V59, P1
  • [4] NELSON BW, 1959, 1ST INT OC C PREPR A, P640
  • [5] Postma H., 1955, DEUTSCH HYDROGRAPH Z, V8, P137
  • [6] PRITCHARD DW, 1952, J MAR RES, V11, P106
  • [7] SCHUBEL JR, 1967, SE GEOLOGY, V8, P85
  • [8] SCHUBEL JR, 1968, CHESAPEAKE BAY I JOH, V35
  • [9] SCHUBEL JR, IN PRESS