TY - JOUR
T1 - Hydraulic conductivity and related physical properties of peat, lost river peatland, northern minnesota
AU - Chason, David B.
AU - Siegel, Donald I.
N1 - Funding Information:
The interrelationships among selected geotechnical characteristics and microstructure for Late Pleistocene glaciolacustrine varved clay from a site in the Elk Valley are presented. Oedometer test results revealed preconsolidation pressures greater than would be expected under the previous maximum overburden cover. The presence of segmented failure envelopes and moderately high liquidity indices suggest the presence of cementation bonding. This conclusion is supported by the porous laminar-matrix microstructure of the varved clay. Natural slope instability is influenced by horizontal seepage within highly permeable interbeds in the clay, the main mode of failure being rotational slumping. Slope failure appears governed by shear strength parameters that are intermediate between those yielded by the over-and normally-consolidated regions of the failure envelope.
PY - 1986/8
Y1 - 1986/8
N2 - We measured hydraulic conductivity (K), bulk density, and humification of peat in three soil profiles at a spring fen-raised bog complex in the Lost River Peatland, northern Minnesota. Piezometers were installed at saturated depths ranging from 0.5 to 3.0 m on a raised bog, its external fen margin, and an adjacent spring fen, and field K was determined by time-lag methods. Field K ranges from 2.5 × 10−4to 5.6 × 10−3cm/s on the bog, from 1.5 × 10−3to 2.6 × 10−2cm/s at the fen margin, and from 6.7 × 10−4to 1.6 × 10−2cm/s on the spring fen. The K determined for partially decomposed peat deeper than 1 m is 2 to 6 times greater than previously reported in the literature. There appears to be little correlation of K with depth, as suggested by most other workers who have investigated only the uppermost “active‘’ layer, about 50 cm deep. Laboratory analyses of K from peat cores show that the ratio of horizontal K (Kh) to vertical K (Kv) is highly variable throughout the peat column. Khis generally one to two orders of magnitude greater than Kv. Bulk density values are similar to those found for other moderately decomposed peats in Minnesota, ranging from 0.06 to 0.14 g/cm3. Bulk density and humicity do not statistically correlate with depth or with K for the peats in the Lost River Peatland. This study suggests that humified peat can transmit groundwater more rapidly than previously thought and that the interaction between groundwater in the peat and associated surface waters can be significant.
AB - We measured hydraulic conductivity (K), bulk density, and humification of peat in three soil profiles at a spring fen-raised bog complex in the Lost River Peatland, northern Minnesota. Piezometers were installed at saturated depths ranging from 0.5 to 3.0 m on a raised bog, its external fen margin, and an adjacent spring fen, and field K was determined by time-lag methods. Field K ranges from 2.5 × 10−4to 5.6 × 10−3cm/s on the bog, from 1.5 × 10−3to 2.6 × 10−2cm/s at the fen margin, and from 6.7 × 10−4to 1.6 × 10−2cm/s on the spring fen. The K determined for partially decomposed peat deeper than 1 m is 2 to 6 times greater than previously reported in the literature. There appears to be little correlation of K with depth, as suggested by most other workers who have investigated only the uppermost “active‘’ layer, about 50 cm deep. Laboratory analyses of K from peat cores show that the ratio of horizontal K (Kh) to vertical K (Kv) is highly variable throughout the peat column. Khis generally one to two orders of magnitude greater than Kv. Bulk density values are similar to those found for other moderately decomposed peats in Minnesota, ranging from 0.06 to 0.14 g/cm3. Bulk density and humicity do not statistically correlate with depth or with K for the peats in the Lost River Peatland. This study suggests that humified peat can transmit groundwater more rapidly than previously thought and that the interaction between groundwater in the peat and associated surface waters can be significant.
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U2 - 10.1097/00010694-198608000-00005
DO - 10.1097/00010694-198608000-00005
M3 - Article
AN - SCOPUS:0022878628
SN - 0038-075X
VL - 142
SP - 91
EP - 99
JO - Soil Science
JF - Soil Science
IS - 2
ER -