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“SEASONAL WATER TABLE AND TEMPERATURE RELA- TIONSHIPS IN CALCAREOUS TILL AND RESIDUAL SOILS OF CENTRAL MAINE” . D. E. Turcotte, USDA-NRCS C.C. Dorion, C.C. Dorion Geol. Svcs. . Coarse-Loamy Sebasticook Catena (introduced in 2008). - PowerPoint PPT Presentation
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“SEASONAL WATER TABLE AND TEMPERATURE RELA- TIONSHIPS IN CALCAREOUS TILL AND RESIDUAL SOILS OF CENTRAL MAINE”
D. E. Turcotte, USDA-NRCSC.C. Dorion, C.C. Dorion Geol. Svcs.
Some-what
Exces-sively
DrainedWell
DrainedWell
Drained
Mode-rately Well
Drained
Some-what
Poorly Drained
Poorly Drained
Very Poorly
Drained
Corinna
LithicDystrudept
Penobscot
Typic Dystrudept
Sebas- ticook **
Dystric Eutrudept
Wassoo-keag
Oxyaquic Eutrudept
Kendus-keag *
Aquic Dystric
Eutrudept
Monarda
Aeric Endoa-quept
Burnham
Histic Humaquept
Shallow (25-49
cm)
Mod. Deep (50-101
cm)
Deep (102-151
cm)
Deep (102-151
cm)
Very Deep
(152+ cm)
Very Deep (152+ cm)
Very Deep
(152+ cm)
Coarse-Loamy Sebasticook Catena (introduced in 2008)
* Series yet to be established (typical pedon yet to be decided on)
Series in bold are the basis of water table study in Central Maine
** Comparable to well drained, very deep Lombard series out of NH
Typical Characteristics of Sebasticook Catena soils
→ Strongly acid to neutral till and/or moderately acid to slightly alkaline residuum of Waterville (and presumably Sangerville) Formation lime- interbedded phyllite, calcareous metasiltstone and pelitic limestone
→ Mapped thus far in towns of Exeter, Corinth, Corinna, Stetson, Newport, Garland and Bradford in Southern Penobscot County
→ Parachanners or decayed rock fragments in till, or paralithic materials or saprolite as residuum
→ Negligible podzolization (even in late successional to climax forest)
→ Minimal O horizon in deciduous or northern white cedar forests
→ Blocky structure and more friable consistence in substratums and/or deeper sola
1985 Bedrock Geologic Map of Maine
Maine Geological Survey
Objectives of Central Maine Water Table Study
1o : testing for moisture regime, pedon classification, and apparent versus perched water tables
2o: a) define each soil’s drainage class; b) evaluate soil temperature early and late in the growing season in the Ap horizons of Wassookeag soils; c) compare the start and end of the growing season based on -2.2 o C or 0 o C frost-free season thresholds, soil temperature @ 10 cm, water temperature in wells, and soil temperature @ 50 cm; and d) compare daytime air temperatures between spring and fall seasons and between field and forest settings
Experimental Design of Central Maine Water Study
> 3 forested somewhat poorly drained Kenduskeag soils on 2-4% slope 3 cropped moderately well drained Wassookeag soils on 1-3% slope
> 2/3rds of sites in the town of Corinth & 1/3rd in the town of Exeter
> pedons described and sampled (for NSSL analyses) in 2002 and sites monitored during spring & fall 2002 - 2005 (two lost in 2004)
> PVC well with perforations @ 15 to 100 cm and PVC piezometer with perforations @ 85 to 100 cm installed at each site
> sites monitored weekly for water tables in wells and piezometers, soil temperature @ 10 cm and 50 cm, water temperature in well, air temperature, and precipitation (via rain guages)
> wet soil at Kenduskeag sites tested with a, a-dipyridyl in 2003
Co-author C.C. Dorion assisting in the description and sampling of Wassookeag pedon on till plain at monitoring site by Countryside Restaurant off Rt. 15 in Corinth
Wells and Piezometers(courtesy of Dr. Jay Bell, Univ. of Minn.)
Well
Water EntersEntire Length
Piezometers
Water EntersEnd Only
PiezometerInstallation
Piezometer
SoilBackfill
BentoniteClay Seal
Sand
Mound
(courtesy of Dr. Jay Bell, Univ. of Minn.)
Bentonite being poured around upper portion of well or piezometer (installed per Sprecher, S.W. 2000. Installing monitoring wells / piezometers in wetlands. U.S. Tech. Note ERDC TN-WRAP-00-02, Army Corps of Eng)
KGEL. Other Eutrudepts that in normal years are saturatedwith water in one or more layers within 100 cm of the mineralsoil surface for either or both:1. 20 or more consecutive days; or2. 30 or more cumulative days.Oxyaquic Eutrudepts
KGEJ. Other Eutrudepts that meet both of the following:1. In one or more horizons within 60 cm of the mineral soil surface, have redox depletions with chroma of 2 or less and also aquic conditions for some time in normal years (or artificial drainage); and2. Do not have free carbonates throughout any horizonwithin 100 cm of the mineral soil surface.Aquic Dystric Eutrudepts
Page 179 of the 11th edition of the Keys to Soil Taxonomy
2002 1,112 Yes + none dry August wet November
2003 1,240 Yes + dry January wet February dry July
wet Septemberwet October
2004 951 Yes - wet December dry January dry March dry June
wet August dry October
2002-2004 MEAN
1,101
2005 1,574 No + wet April wet May
very wet October (362 millimeters)
1971-2000 MEAN, S.D.
1,088 + / - 159(929 to 1,247)
Corinna Daily NOAA Climatic Station ANNUAL 1 ABNORMALLY 3 ABNORMALLY 3
PRECIPI- WET OR DRY WET OR DRY TATION NORMAL MONTHS MONTHSYEAR (millimeters) YEAR? 2 (DEC. – JULY) (AUG. – NOV.)__________________________________________________________________________________
1 based on sum of December – November monthly totals2 Soil Survey Staff, 20103 Outside of the standard deviation of the 30 year mean for that month
Spring 2002 Fall 2002 Spring 2003 Fall 2004
Route 15, Corinth 2% slope(2% faint deple-tions @ 66cm +)
* 7-13 days May 1 to 7-13(to 89 cm)
none (to 100 cm)
** 7-9 daysMay 3 to 9-11(to 94 cm)
*** none (to 96 cm)
upper Beans Mill Road, Corinth1% slopes(2% prominent concetnrations @ 89cm +)
* 7-13 days May 1 to 7-13 (to 99 cm)
none (to 98 cm)
** none (to 100 cm)
*** 17-19 daysSept. 19 to Oct. 5-7(to 89 cm)
Route 43, Exeter, 3% slopeno redox above saprolite (in @ 61 cm)
* 29-35 days Apr. 24 to May 22-28(to 91 cm)
*** none (to 100 cm)
* 16 days May 4 to May 19(to 91 cm)
pipes abolished by machinery
Water tables in monitoring wells above 100 cm during normal precipitation seasons at Wassookeag sites during growing season based on soil temperatures above biological zero (5o C) @ 50 cm
* water table was present within 100 cm when growing season commenced** water table was present within 100 cm before growing season commenced*** water table was present within 100 cm at least 13-15 days after growing season concluded
Wassookeag pedon at Exeter cropland site off of Route 43 (described and sampled on May 21, 2002)
2C1 saprolite: 61-73 cm
2C2 saprolite: 73-119 cm(increase in < 2 chroma lithochromic in nature)
Spring 2002 Fall 2002 Spring 2003 * Fall 2004
lower Beans MillRoad, Corinth, 4% slope
66 days May 6 – July 10
5 daysNov. 15-19
54 days May 2 – June 24
11 and 51 daysSept 20-30Oct. 14 – Dec. 3
upper Beans Mill Road, Corinth, 2% slope
38 and 4 daysMay 8 – June 14June 27-30
2 daysNov. 20-21
49 daysMay 5 – June 22
19 daysNov. 25 – Dec. 13
by French Stream, Exeter, 2% slope
14 daysMay 8 -21
2 daysNov. 22-23
10 and 20 daysMay 9-18May 29 – June 17
14 daysNov. 26 – Dec. 9
Water tables in monitoring wells at the Kenduskeag sites that rose above 40 cm depth during normal precipitation seasons when well water was > 5o C
* Out of 48 applications in this season and in the following (abnor- (mally wet) fall, on only one occasion was there a positive reaction to alpha,alpha-dipyridyl (as a test for an aquic moisture regime)
Redoximorphic features in clod from Kenduskeag pedon >>>
Decayed fragments in clod from Kenduskeag pedon >>>
Perched Water Table (courtesy of Dr. Jay Bell, Univ. of Minn.)
Soil
Saturated
Aquitard
Substratum
? (Unsaturated)
(Unsaturated)
* In one instance (5% frequency) there was water in the well (at 92 cm) below the top of the substratum while there was no water in the piezometer.
Growing Season Basis 2002 2003 2004 2005 Mean / LengthFrost-Free> 0o C
May 23 to October 3
May 18 to October 5
May 9 to October 5
May 15 to October 20 ****
May 16 to October 8(146 days)
Frost-Free > -2.2o C
April 29 to October 8
May 5 to October 19
April 30 to October 5
April 23 to October 21
April 29 to October 13 (168 days)
Wassookeag * sites’ soil temperature > 7.2o
C @ 10 cm **
May 2 to October 20(178 days)
Wassookeag * sites’ soil temperature > 5o C @ 50 cm
April 29 to November 4
April 30 to November 13
April 30 to November 12
April 24-25 to November 21
April 28 to November 12(199 days)
Kenduskeag * sites’ soil temperature > 5o C @ 50 cm
May 3 to November 19
May 8 to December 4
April 30 to November 26
data incomplete May 4 to November 26(207 days)
Kenduskeag * sites’ water temperature > 5o C ***
May 7 to November 21
May 5 to November 27
April 30 to December 8
April 24 to December 2-3
May 2 to November 30(213 days)
Growing season comparisons based on Corinna air temperature lows (and soil or water temperatures from averaged Kenduskeag or Wassookeag sites)
* Exeter sites not monitored in Fall 2004 and 2005 (Wassookeag) or just 2005 (Kenduskeag)
CONCLUSIONS1) water table and soil temperature data support moderate well to well drainage and the oxyaquic subgroup for the Wassookeag series
2) water table and soil temperature data and negative a, a-dipyridyl reactions support somewhat poor drainage and the aquic dystric subgroup for the Kenduskeag series
3) though the upper site was flatter, heavier textured and close to a hydric map unit, the lower landscape position Kenduskeag site in Corinth was consistently wetter
4) water table observations in the wells and piezometers at the Corinth Kenduskeag sites suggest that water tables are apparent
5) growing seasons based on air temperature or plow layer temperature were comparable to those based on soil temperature @ 50 cm or well water temperature in the spring, but not so in the fall when they ended much sooner
6) afternoon air temperatures were significantly cooler in the fall seasons than in the spring seasons, but forested sites were not cooler than field sites
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