HomeMy WebLinkAbout14 Development Permit 305 TAMU Well 2FILE NOTE
Date: October 16, 1995
To: DDP File No. 305: TAMU Well No . 2
From : Steve Homeyer . -~
Graduate Engineer o/
There is not a DDP for this well due to it being located on the TAMU
Campus. However, a drainage report was conducted for this well by Kling
Engineering.
DRAINAGE REPORT
FOR
TAMU WELL NO. 2
UNION PACIFIC RESOURCES COMP ANY
J. E. Scott Survey, A-50
College Station, Brazos County, Texas
September 12, 1995
DEVELOPED BY:
Union Pacific Resources Company
clo Duane Phillippi
7300 N. F.M. 2818, Suite 200
Bryan, TX 77803
( 409)778-4867
PREPARED BY:
Kling Engineering & Surveying
4103 Texas Avenue, Suite 212
Bryan, TX 77802
(409)846-6212
Drainage Report
for
TAMU Well No. 2
Union Pacific Resources Company
J. E. Scott Survey, A-50
College Station, Brazos County, Texas
September 12, 1995
GENERAL LOCATION & DESCRIPTION
The proposed drilling site for TAMU #2 is located within the White Creek Drainage Basin
approximately 800' southwest of Agronomy Road approximately 1900' northwest of the
intersection of University Drive and Agronomy Road. (See Appendix 3: "Vicinity Map"). For
impact purposes this well is considered to be high. Currently 1/2 of the site is plowed cropland
with no vegetation, and the other 1/2 is pasture land with a small tin building, some barbed wire
fencing and a few power poles. The site is relatively flat with a slight slope to the southwest.
There are two earth channels that help facilitate drainage of this area. Proposed improvements
consist of constructing a 330' x 230' crushed limestone drilling pad and constructing an access
road from Agronomy Road to the drilling pad.
DRAINAGE BASINS & SUB-BASINS
The primary drainageway for this site is White Creek Tributary "C". Runoff proceeds as
overland flow until it is interrupted by one of the two earth channels. Both of these channels drain
into a series of swales and roadside ditches within the TAMU Research Center until ultimately
discharging into White Creek Tributary "C". Neither the proposed drilling pad nor the proposed
access road lies within the 100 year floodplain according to the Flood Insurance Rate Map for
Brazos County, Texas, and Incorporated Areas (See Appendix 2: "Flood Plain Map").
Two primary studies have been performed on White Creek and its tributaries. The first
is a study performed by the Federal Emergency Management Agency in July, 1992, titled El.oo.d.
Insurance Study -Brazos County, Texas and Incorporated Areas. The purpose of this report was
to investigate the existence and severity of flood hazards for Brazos County and to aid in the
administration of the National Flood Insurance Act of 1968 and the Flood Disaster Protection Act
of 1973. The second study is the Stormwater Management Plan, Phase III, performed by Walton
and Associates -Consulting Engineers, Inc. contracted with the City of College Station in 1987.
The purpose of this study was to gain knowledge of the existing and future drainage conditions
in the City and to identify flood problems and flood prone areas.
DRAINAGE DESIGN CRITERIA/FACILITY DESIGN
A topographic/grading plat was prepared to show existing conditions, the limits of the
proposed improvements, and to show the secondary drainageways that will drain the site (See
Appendix 4: "Topographic/Grading Plat -Kling Engineering) (See note 2, Appendix 4).
TAMU Well No. 2
Drainage Report Page 2
The well pad will be divided at the well head to drain in opposite directions. The northerly
portion will sheet flow off the pad into the earth channel running parallel to the pad and leave the
site following the path shown on the topographic/grading plat which ultimately drains into White
Creek Tributary "C". This drainage path will be referred to hereafter as "Path 1 ". Runoff that
proceeds as sheet flow off the well pad in a southerly direction will drain through the adjoining
field to the southeast of the pad where it will be intercepted by an existing channel that flows in
a southwesterly direction, then proceeds following the path shown on the plat which ultimately
drains into White Creek Tributary "C". This path will be referred to hereafter as "Path 2". There
will be no off-site runoff onto this tract. The earth channel along the northwest line of the pad
intercepts any flow coming from the area north of the pad site.
The Rational Method was used to determine the increase in runoff expected for this
development. The design storm used was the 25 year event. A runoff coefficient of 0.25 was
used for pre-developed conditions and 0.85 was used for post-development conditions which
produced the following results:
Entire Well Pad
Northerly portion
Southerly portion
Acreage
(acres)
1.77
0.93
0.84
Ere02s
(cfs)
4.36
2.29
2.07
£Qs1Q25 Increase
(cfs) (cfs)
14.83 10.5
7.79 5.5
7.04 5.0
The northerly portion affects "drainage Path #1", the southerly portion affects "drainage
Path #2", thus an increase of 5.5 cfs is expected for Path #1 and an increase of 5.0 cfs is expected
for Path #2.
The drainage areas impacted by this development are shown on the plat entitled Drainage
Areas of TAMU #2 (See Appendix 5: Drainage Areas). Using the Rational Method and Mannings
Equation, post development runoff calculations were performed for each drainage area and its
corresponding drainage structure (See Calculations: Appendix 7).
A tabulation of the results for each drainage area follows:
Drainage Area
#1
#2
#2A
Area
(acres)
17.7
11.5
5.1
Q 25 E.!2.s1 Drainage
(cfs) Structure
64.6 4 -30" RCP
47.6 2 -30" RCP
22.6 2 -24" RCP
Structure
Capacity
146.7
97.1
40.5
From the table it can be seen that for each drainage area the runoff from the 25 year storm
event (Q25 -Post) is substantially less than the drainage capacity for the same area (Column 5).
Therefore, the proposed development will not increase runoff to a level above the carrying
capacity Of the drainage structures mentioned above.
TAMU Well No. 2
Drainage Report Page 3
To analyze both drainage paths, the following steps were taken: 1) field measurements
were taken so as to define the channel cross-section at different segments along each path, 2)
channel capacity for each segment was determined, 3) the area contributing to each segment was
delineated, 4) using Mannings Equation, a Q25 for each area was calculated, and the results
compared . To analyze drainage path #1, the path was broken into segments , i.e. segments A-B,
B-C, and C-D, as shown on Appendix 5 . The corresponding areas affecting each channel lA, lB
and IC respectively are shown on the same plat. To analyze drainage path #2, the path was
broken into segments E-F. The results are tabulated below:
.Drainage Path #1
Segment
AB
BC
CD
Drainage Path #2
Segment
EF
CONCLUSIONS
Q25 -Post (cfs)
11.1
16.6
27.9
Q25 -Post
22.6
Capacity (cfs)
33 .3
109.2
56.2
Capacity
190.0
TAMU #2 is considered to be a "high" impact well, and the drainage analysis has been
performed accordingly. The 25 year storm was used as the design storm . An increase in flow in
the secondary drainageways is expected, but does not exceed the drainage capacity of either of the
studied drainageways.
"I hereby certify that this report (plan) for the drainage design of the IAMU Well No.2
was prepared by me (or under my supervision) and that proper engineering considerations were
taken into account for the owners thereof, II ~,,,,,,, .'
.........-.-. ......... -;¢. F ti \' ~· ~ . .. ...
:'\> • •• :t
;·
TAMU Well No. 2
Drainage Report Page 4
APPENDICES
1) General Location Map -U.S. G . S. Quad
2) Flood Insurance Rate Map -FEMA
3) Vicinity Map
4) Topographic/Grading Plat -Kling Engineering
5) Drainage Areas -Kling Engineering
6) Calculations -Rational Method
7) Calculations -Mannings Equation
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APPENDIX 6
CALCULATIONS -RATIONAL METHOD
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100 SHEETS
200 SHEETS
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Project Description
Project File
Worksheet
Flow Element
Method
Solve For
Input Data
Mannings Coefficient
Channel Slope
Diameter
Results
Depth
Discharge
Flow Area
Wetted Perimeter
Top Width
Critical Depth
Percent Full
Critical Slope
Velocity
Velocity Head
Specific Energy
Froude Number
Maximum Discharge
Full Flow Capacity
Full Flow Slope
Drainage Area #1: 4 -30" RCP's
Worksheet for Circular Channel
d:\fmw\tamu#2 .fm2
4-30" RCP's@ TAMU#2
Circular Channel
Manning's Formula
Full Flow Capacity
0.013
0.008000 ft/ft
2.50 ft
2.50 ft
36 .68 ft3/s
4.91 ft2
7.85 ft
0.00 ft
2.05 ft
100 .00 %
0.007978 ft/ft
7.47 ft/s
0.87 ft
FULL ft
FULL
39 .46 ft3/s
36 .68 ft3/s
0.008000 ft/ft
APPENDIX 7
CALCULATIONS MANNING'S
Kling Engineering & Surveying
EQUATION
Sep 7 , 1995
09 :41 :47 Haestad Methods, Inc. 37 Brookside Road Waterbury, CT 06708 (203) 755-1666
FlowMaster v4 .1 c
Page 1of1
Project Description
Project File
Worksheet
Flow Element
Method
Solve For
Input Data
Mannings Coefficient
Channel Slope
·Diameter
Results
Depth
Discharge
Flow Area
Wetted Perimeter
Top Width
Critical Depth
Percent Full
Critical Slope
Velocity
Velocity Head
Specific Energy
Froude Number
Max imum Discharge
Full Flow Capacity
Full Flow Slope
Drainage Area #2: 2 -30" RCP's
Worksheet for Circular Channe l
d:\fmw\tamu#2.fm2
Drainage Area #2
Circular Channel
Manning's Formula
Full Flow Capacity
0.013
0.014000 tuft
2 .50 ft
2.50 ft
48.53 ft3/s
4.91 ft2
7.85 ft
0.00 ft
2.28 ft
100.00 %
0.012209 ft/ft
9.89 ft/s
1.52 ft
FULL ft
FULL
52.20 ft3/s
48 .53 ft3/s
0.0140 00 ft/ft
Kling Engineering & Surveying Sep 7 , 1995
09:54:27 Haestad Methods, Inc. 37 Brookside Road Waterbury, CT 06708 (203) 755-1666
FlowMaster v4.1 c
Page 1 of 1
Project Description
Project File
Worksheet
Flow Element
Method
So lve For
Input Data
Mannings Coefficient
.Channel Slope
Diameter
Results
Depth
Discharge
Flow Area
Wetted Perimeter
Top Width
Critical Depth
Percent Full
Critical Slope
Velocity
Velocity Head
Specific Energy
Froude Number
Maximum Discharge
Full Flow Capacity
Full Flow Slope
Drainage Area #2A: 2 -24" RCP's
Worksheet for Circular Channel
d:\fmw\tamu#2.fm2
Drainage Area #2A
Circu lar Channel
Manning's Formula
Full Flow Capacity
0.013
0.008000 ft/ft
2.00 ft
2.00 ft
20 .23 ft3/s
3.14 ft2
6.28 ft
0.00 ft
1.61 ft
100 .00 %
0.008226 ft/ft
6.44 ft/s
0.64 ft
FULL ft
FULL
21.76 ft3/s
20.23 ft3/s
0.008000 ft/ft
Kling Engineering & Surveyi ng Sep 7, 1995
09:48 :59 Haestad M ethods, Inc. 37 Brookside Road Waterbury, CT 06708 (203) 755-166 6
FlowMaster v4 .1 c
Page 1 of 1
DRAINAGE PATH #1 -SECTION "A-8"
Worksheet for Irregular Channel
Project Description
d:\fmw\tamu22 .fm2 Project File
Worksheet
Flow Element
Method
DRAINAGE PATH #1 -SECTION "A-8"
Irregular Channel
Manning's Formula
Solve For Discharge
Input Data
Channel Slope 0.010000 ft/ft
Water Surface Elevation 351 .50 ft
Elevation range: 350 .50 ft to 351.50 ft.
Station (ft) Elevation (ft)
0 .00 351 .50
8.00 350 .50
10 .00 350 .50
18.00 351 .50
Results
Wtd. Mannings Coefficient 0.030
Discharge 33.32 ft3/s
Flow Area 10 .00 ft2
Wetted Perimeter 18 .12 ft
Top Width 18 .00 ft
Depth 1.00 ft
Critical Water Elev. 351.40 ft
Critical Slope 0.016623 ft/ft
Start Station
0.00
Velocity 3.33 ft/s
Velocity Head 0.17 ft 351 .4 \
Specific Energy 351.67 ft
Froude Number 0.79
Full Flow Capacity 33 .32 ft3/s
Flow is subcritical.
351 .3
351 .2
351 . 1
351 .0
350. 9
350. 8
350. 7
350. 8
5 350.
0 .0
\
\
\
\
2 .0
Kling Engineering & Surveying
End Station
18 .00
\
I\
\
\
[\
\
4 .0 6 .0
~ ..
\
Roughness
0.030
I v
/
7
I
I
I v
I
I
I/
I
8 .0 10.0 12.0 14.0 16.0 18
Station (ft)
Sep 11, 1995
21 :57:53 Haestad Methods, Inc. 37 Brookside Road Waterbury, CT 06708 (203) 755-1666
FlowMaster v4 .1 c
Page 1of1
DRAINAGE PATH #1 -SECTION "B-C"
Worksheet for Irregular Channel
Project Description
untitled Project File
Worksheet
Flow Element
Method
DRAINAGE PATH #1 -SECTION "B-C"
Irregular Channel
Manning's Formula
Solve For Discharge
In put Data
Channel Slope 0.012000 tuft
Water Surface Elevation 349 .68
Elevation range: 348 .41 ft to 349 .97 ft .
Station (ft) Elevation (ft)
0.00 349 .97
74.00
92.00
106 .00
153 .00
Results
Wtd. Mannings Coefficient
Discharge
Flow Area
Wetted Perimeter
Top Width
Depth
Critical Water Elev.
349.46
348.41
349.22
349 .68
0.0 30
109 .19
39 .84
110 .98
110.92
1.27
349.61
tt3/s
ft2
ft
ft
ft
ft
Critical Slope 0.018641 tuft
Velocity 2.74 tus
Velocity Head 0.12 ft
Specific Energy 349.80 ft
Froude Number 0.81
Full Flow Capacity 270 .31 tt3/s
Flow is subcritical.
ft
Start Station
0 .00
350.0
349.8
~~
349.6
349.4
E.
349.2
349.0
348.8
348.6
End Station
153 .00
~
""'-" I"\
\
Roughness
0 .030
'""" ..
/v
I
\ I
\ I v
I
-
/
/ I
/
'
I
348.4
0 .0 20.0 40.0 60.0 80.0 100.0 120.0 140.0 16(
Sep 11 , 1995
18:49:04
Station (ft)
Kling Engineering & Surveying
Haestad Methods, Inc. 37 Brookside Road Waterbury, CT 06708 (203) 755-1666
FlowMaster v4.1 c
Page 1of1
DRAINAGE PATH #1 -SECTION "C-D"
Worksheet for Irregular Channel
Project Description
Project File
Worksheet
Flow Element
Method
Solve For
Input Data
untitled
DRAINAGE PATH#1 -SECTION "C-D"
Irregular Channel
Manning's Formula
Discharge
Channel Slope 0.010000 ft/ft 1
Water Surface Elevation 34 7. 77 ft
Elevation range: 346 .81 ft to 348.44 ft .
Station (ft) Elevation (ft)
0.00 348.44
Start Station
0.00
38 .00
49.00
57 .00
74 .00
130 .00
Results
Wtd . Mannings Coefficient
Discharge
Flow Area
Wetted Perimeter
Top Width
Depth
Critical Water Elev.
Critical Slope
Velocity
Velocity Head
Specific Energy
Froude Number
Full Flow Capacity
347 .82
346 .83
346 .81
347 .62
347 .77
0.030
56 .17
26 .14
91 .51
91.44
0.96
347 .55
ft3/s
ft2
ft
ft
ft
ft
0.017015 ft/ft
2.15 ft/s
0.07 ft
347 .84 ft
0.7 1
411 .16 ft3/s
348.6
348.4
348.2
348.0
Flow is subcritical. _____________________ g 347.8
347.6
347.4
347.2
' ~
'\
End Station
130 .00
"' ~
\
\
\ I
Roughness
0.030
...
,...-L---
I
I
L---.......
347.0 l1
Sep 11 , 1995
18:37:29
346.8
0 .0 2 0 .0
Kling Engineering & Surveying
40.0 60.0 80.0
Station (ft)
Haestad Methods, Inc. 37 Brookside Road Waterbury, CT 06708 (203) 755-1666
100.0 120.0
FlowMaster v4.1 c
Page 1 of 1
140
DRAINAGE PATH #2 -SECTION "E-F"
Worksheet for Irregular Channel
Project Description
d:\fmw\tamu22.fm2 Project File
Worksheet
Flow Element
Method
DRAINAGE PATH #2 -SECTION "E-F"
Irregular Channel
Manning's Formula
Solve For Discharge
Input Data
Channel Slope 0.008000 ft/ft
Water Surface Elevation 345.42 ft
Elevation range: 343 .99 ft to 347.63 ft.
Station (ft) Elevation (ft)
0.00 347 .63
38 .00 346 .72
65.00 344.12
68.80 343 .99
72 .20 344.05
85 .20 344 .61
154 .20 345.42
Results
Wtd . Mannings Coefficient 0.030
Discharge 190 .00 ffl/s
Flow Area 60.84 ft2
Wetted Perimeter 102 .78 ft
Top Width 102.70 ft
Depth 1.43 ft
Critical Water Elev . 345 .27 ft
Critical Slope 0.016275 ft/ft
Velocity 3.12 ft/s
Velocity Head 0.15 ft
Specific Energy 345 .57 ft
Froude Number 0.72
Full Flow Capacity 2356 .82 ffl/s
Flow is subcritical.
Start Station
0.00
348.0
347.5 ......
347.0
346.5
g346.0
3 45 .5
3 45.0
344.5
344.0
~ ~
End Station
154.20
~
\
\
\
\
Roughness
0.030
..
/" ~
\//
~ v-
I
343.5
0 .0 20.0 40.0 60.0 80.0 100.0 120.0 140.0 160
Sep 11, 1995
22:05:51
Station (ft)
Kling Engineering & Surveying
Haestad M et hods, Inc. 37 Brookside Road Waterbury, CT 067 08 (203) 755-1666
FlowMaster v4.1 c
Page 1 of 1
~-~ r Cl~~ o<?c~s S:~!lEG1~1 ~!~~!~N ~ College Station, Texas 77642-9960
August 16, 1995
Kling Engineering and Surveying
4103 Texas Avenue, Ste. 212
Bryan, TX 77802
Attn : B.J. Kling
Dear Mr. Kling :
( 409) 764-3500
I have reviewed the drainage report for TAMU Well No. 2 that you prepared for Union
Pacific Resources Company, dated June 29 , 1995. I am disappointed in this report . All it
tells me is that when the well pad is built, more water will run off the site than before the
pad was built . I do not need a drainage report to tell me that.
You state several times in the report that this is considered a high impact report. I agree
with this statement and have conveyed that to Mr. Bruchez's office . Since this is a high
impact location, your report should address what impacts the additional runoff will have
on the surrounding area and existing drainage facilities . It should also address what
improvements should be made to mitigate these impacts. There should be a plan in the
report showing where and how these improvements are to be constructed . Your report
does none of that.
Please resubmit your report in a more thorough form that addresses the concerns stated
above .
Sincerely,
Kent Laza
City Engineer
cc : j Veronica Morgan, Asst. City Engineer
Duane Phillippi
Ernest Bruchez
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