K
r aig DM
a rquis An In v e sti
gati
o ni
nto theSo u r c e s o
f
W
ate rQ
u al it
y I m pairm
e nt ina
Sm
al l
De v elo
p
ed
W
ate r she
d
T
h
ein v e s
ti g
atio n e x amin e
d
the
chemic a
l
w ate rq
u al it
yin
M
e eti
ng
of
th
eW
ate r sC
r e ek
, a smal l
str e am tha
tp
r ed
om i
n a ntl
ydr a
i
n s th
eU
niv e r s
i
ty of N
o rth
C
a r oli
n a atC h
ap
el H i l l
c amp
u s Phy
si
c al
a nd
ch
em i
c al p
a r amete r sw
e r e mo nit
o r ed fo r
b
oth dr
yw
e athe r
a nd
sto rm
e v e nt c o nd it
io n s
i
n o rd
e r tod
ete rm i
ne the
im
p
a ct s of
p
oi
nt a nd
nonpoin
t so u r c e s of
pol lu t
io n
P
oi
nt s o u r c e s of d
om
e sti
cw
a stew
ate r, sp il l
s,a n
d
u ni d
e nti fi
ed in
putsw
e r ed
ete cted
thr o u
g h
o ut th
e c o u r s e of
the stud
y Th
ec o r r e ct
iv e
m
e a s u r e si
m p leme nted
,b
oth
str u ctu r al
r ep
air s
tol
e ak i
ng
s ew
e rl i
n e s a nd
po
l i
cy cha ng
e s,h
a v e sin c e
i
m pr o v ed
theb
a s el i
n e chem i
c al w
ate rq
u al it
y of
th
e c r e ek
N
o c o r r e ctiv e
me a s u r e s,h
owe v e r , we r e em
plo
yed
t om i
tig
ate th
eh
yd
r ol
ogi
c o rpo
llu
ta ntlo a
d in
g eff
e cts of
sto rm
w ate r r u n of f
T he r e
f
o r e, th
e c r e ek
c o ntin u e s
tob
ei
mp
a cted b
y sto rm
e v e nt r el
ated
str e am b
a nk
s c o u r, s ed im
e nt
i
nputs, a nd
el
e v ated
po
l l
uta nt c o n c e ntr atio n s a n
d l
o ad
sT h
e s e r e s ul
ts s ug g
e st th
at th
eb i
olo
g i
c al in
teg ri
tyo
f
th
e c r e ek
r emain s
im
p
air e
d
, a nd
th
atlit t
l
ei f
a nyi m
pr o v em
e nti
nE
P T ta x ari
chn e s s
I
. IN
TR O D U C T I O N
1A
Hi
sto ry of
th
eC
r e ek
a n dW
ate r shed
1B .
C h
ara cte ri
s ti
cs of
th
eN
atu ral
W
ater shed
2C
T h
e Re s e a r ch Stu
d
y 8n
.L I
TE R A
TU R E R E V I E
W
9A
Reg
ul
ati
ng
W
ate rQ
u ali
t y9
B .
T h
eI m p
a cts of
aD
e v elo
p i
ng
W
ate r sh
ed
1 0C
L
a nd U
s eC h
a ng
e s 14D
C h
em i
c al
a nd P h
ysic al P
a ram
ete r s19
E
N
o np
oin
tSo u r c e
Poll
utio
n 2 5F
P
oi
ntSo u r c e
P
ol l
uti
o n 2 7G U
rb
anB
e stM
a n ag
em
e ntP
r a ctic e
s 2 8H
T h
eR
e s e a r ch St
udy
3 2I Re s e a r c
h O b
j
e ctiv e s
3 4m
.M
ET H O
DS
3
5A
.W
ate r sh
ed D
e s c ri
p ti
o n 3 5B
Sa
m p l i
ng S
tatio n s
38
C
F i
el d D
ataC
ol l
e ctio n
4
01
Sa
m pl i
ng
4
02
F l
ow
M
o ni
tori
ng 41
3
F ie
l d A
nal
ysi
s4 3
D .
L
ab
o r ato ry A
n al
ys e s 43
1
N it
r ate a nd N i
tri teN i
tr oge n 44
2. A
m
m
o ni
aN i
tr og
e n 44
3 Tota
l
Ph
o sp h
o r u s 4 44
C hl
ori d
e 4 45 Tu r
b i d i
t y 4 46
pH
45
7
C
e rtif i
ed L
ab
o r ato ry A
n al
ys e s 45
A
B a s el i
n eSa
m p l i
ng R
e s ul
ts 4 81 F
i
el d P
a r am
ete rs 4 82 B a s e
li
n e F low
s 5 53 L a
b
o r ato ry Pa r am
ete r s 5 6B
I m p
r o v ed
W
ate rQ
u al i
ty
atSit
e 1 6 9C
Su
p p l
em
e ntal
W
ate rQ
u al i
tyM
o nit
o ri
ng
76
D
St
o rm
Ev e ntS
am p l
e s 7 71
St
o rm w
ate r Pol l
uta ntL
o ad
s 7 72
Y
e a rl y L
o ad i
ng
Rate s 9 1V
. D ISC
US SI
O N
1 0 3A
W
ate rQ
u alit
yIm p
a cts 1 0 31 L o
w
Fl
ow Sa
m p l
e s 1 0 32
St
o rm E
v e ntSa
m p l
e s 1 0 7B
B i
olo
g i
c al I m p
acts 109C
I m p l
em
e nted C
o r r e ctiv e
M
e a s u r es 1 1 0D
B
M
Ps toCo
n si d
e rf
o rC
o ntin u ed
W
ate rQ
u al it
y Im
pr o v em
e nt 1 14V I
.C O N C L U SI O
NS A N
DR E C O
M
M
EN D A T
IO N S
1 1 7A
Stu
d
yC
o n cl
u si
o n s 1 1 7B
F
utu r eW
ate rQ
u alit
yC
o n sid
e r ati
o n s a nd
Re c om m
e nd
ati
o n s 1 1 9V
n
. R E FE R
E NC
ES C
IT
E D 12 1V
m
. AP P E N D I
X 1-
M
a
p
1(
St
ud
y Regio n
)
D C
.A
P PE N
DI X
2 -B
e nthi
cSt
ud y
(
19
9 3)
X
.A
P P E N D I X 3 -D
atalo
g g
e r(
B D R-3 2 0X L
A P
PE N
DI X
4 -F i
e
l d Sh
e ets and N C S
u rf
ac eW
a te rSt
a nd
a rd
sX n
. A P P EN
DI X
5-
St
o rm
Ev e nt Lo ad
o gr aph
sX
m
.A
P PE N D I X
6-
St
o r
m E
v e ntR
eg
res si
o n An al
yse sX I V
.A
P PE N D I X
7-
S
u
p p l
em
e ntal A q
uaT
e ch D
ata(
S it
e 6)
X V
. A P P EN
D IX
8-
R
L I
ST
O
F T A B L E
S
1 Su
m m
a ry of C hapelH
i l lW
e athe r Data(
1 9 4 8 to 1 9 9 4)
42
S
el
e cted
M
ed i
a nE
M
C
sfr
om N U
R P(
U SE
P
A, 19
8 3)
a nd
M
i l l
s(
19
8 2)
2 73
B
e nthi
cM
a c r oi
n v erteb
r ateS
um m
a ryS
tati
sti
c sC
ol l
ec ted i
nA p
ri l
, 1 9 9 33 3
4.
P h
ys
i
c al C h
a r a cte ri
sti
c s Reco rd
ed i
nA p
ri l
, 1 99
3 3 35 B a s
i
nA
r e a s3
86
A
v e r ag
e Dai l
yS
tr e am
Fl
ow
s5
57
S
um m
a ry
of F i
el d P
a r am
eter sfr
om C h
ap
el H i l l St
o rm w
ate rP
r og
r am
76
8
S
um m
a ry of
Lab
o r ato ry Pa r am
ete r sfr
om C h
apel H i l l P
r ogr am
7 69
Si
te 2S
to rm S
am p l i
ng
Ev e nts9
11
0
Si
te 4S
to rm S
am p l i
ng Events9
21 1
Y
e a rl
yT
otal
sf
o r Ba s eli
n e a nd S
to rm E
v e ntL
oad
s 1 0 21 2
Y
e a rl
yP
oll
u ta ntL
o ad i
ng R
ate sf
o rSi
te s 2 a nd
4 1 0 21 3 L a n
d U
s eD
ataF
r om
Pi
ed m
o ntS
tud y Si
te s and
M
e eti
ng
of
th
eW
ate r s 1 0 41 L o c at
i
o n of O
r a ngeC
o u ntyi
nN
o rthC
a r oli
n a 32
G
e o ch
em i
c al
Zon e s of N
orth C
a r oH
n a 63
W
atershed S
oi l S
eri
e sM
ap
7
4
C
ha ng
e si
nW
ate r sh
ed H
yd
r ol
og
y a s a Re s ult
of U
rb
a ni
z ati
on 125
W
ate r sh
ed A
r e a a nd S
oi l
Pe rm
e abi l i
tyR
e stri
c ti
o nsf
o rB
M
Ps 3 06
O
th
e rC
omm
o n R e stri
cti
on s o n BM
Ps 3 17
M
e eti
ng of
theW
at er s -S
ubb
a si
n s and S
am p l i
ng S i
tes3 6
8
St
o rm w
ate rD
r ai
nag
eS
ys tem
3 79
A
v e rag
eT
em p
er atu r e - L ow F l
ow S
am p l
e s 4 91 0
A
v e rag
eC
o nd
u cti
vit
y -L
ow F l
ow S
am p l
e s5
11 1
A
v e r ag
eI
DS C
o n c e ntr ati
o n s -L
o
w F l
ow S
am p l
e s 5 212 Av e r a
g
e DO C
o n c e ntr ati
o n s - Lo
w
Fl
ow S
am
pl
e s 5 31
3
A
v e r ag
e DO
%
S
atu r ati
o n -L
ow
Fl
ow S
am p l
e s 5 41 4
A
v e r age Dail
ySt
ream F l
ow
-Si
te 2
5
71 5
A
v e r age D ail
ySt
r e am
F low
- S ite 4 5 81 6
A
v e r ag
e T u rb i d i
ty -L
ow
F lo
w S
am p l
e s5
91 7
A
v e rag
eA m m
oni
a-N C
o n c e ntr at
i
o n s -L
o
w F l
ow S
am p l
e s6
01 8
A
v e rag
eA m m
oni
a-N L
oad
s -L
ow F l
ow S
1 9 Av e r a
g
eN i
tr ate& N i
tri
te-N C
o n c e ntr ati
ons -L
ow F l
ow S
am p
le s 6 32 0
A
v erag
eN i
trate& N i
tri
te-N L
o ad
s -L
ow F l
ow S
am p l
e s 6 42
1A
v e r ag
eT
otal
Ph
o sp h
o r u sC
o n c e ntr atio n s - L ow F l
ow S
am p l
es 65
2 2
A
v e r ag
e Ph
o sph
o r u s L o ad
s -L
o
w
Fl
ow S
am p l
e s 66
2 3
A
v e r ag
eC hl
o ri d
eC
o nce ntr atio n s
-L
ow
Fl
ow Sa
m p l
es6
72 4
A
ver ag
eC hl
o ri d
eL
o ad
s -L
ow F l
ow Sa
m
p
le s
68
2 5
C
o nd
u ctiv
it
y -Si
te
1
7 12 6
C hl
ori d
eL
oad
-Sit
e1
7 22 7
A
m
m
o ni
a-N L
o ad
-Sit e
1 7 32 8
N i
tr ate& N i
tri
teL
o ad
-Si
te 1 7 4
2
9
T
otal
Ph
o sp h
o r u sL
o ad
-Si
te 1 7
5
3
0A m m
o ni
a-N St
orm L
oad
-Si
te2
78
3
1
N i
tr ate-N St
o rm L
o ad
-Sit
e 2 7 93 2
T
PSt
o rm
Lo ad
-S it
e 2 8 0
3 3
C hl
ori d
eSt
o rm L
o ad
-Si
te 2
8 1
3 4
A m m
o ni
a-N St
o rm
L o ad
-Si
te 4 8 23 5
N it
r ate-N St
o rm
Lo ad
-Sit
e 4 8 33 6
T
PSt
o rm L
o ad
-S i
te 484
3 7
C hl
ori d
eSt o
rm L
oad
-Si
t e 4
8 5
3 8
C
o nd
u ctiv
it
y -Si
te 2 8 73 9.
C
o ndu c
tivit
y -Si
t4 0
T
u rb i d i
ty -Si
te 2 8 94 1
T
u rb i d i
ty -Si
te 49 0
4 2
Sit
e 2 - Am m
o nia
-N S
to rm
Lo ad Regr e s sio n 9 44 3
Sit
e 2 -N i
tr ate
& N it
ri
te-N S
t orm
L o ad
Reg
r e s si
o n9 5
4
4
Si
te 2 -T
otal P h
o sp h
o r u sSt
o rm L
o ad R
eg
r e s si
o n96
4 5
Sit
e 2 -C hl
ori d
eS
to rm L
o ad R
eg
r e s si
o n 9 74 6
Sit
e 4 -A m m
o nia
-N St
o r
m L
o ad R
eg
r e s si
on 98
4 7
Sit
e 4 -N it
r ate& N i
tri
te-N St
o rm L
oad R
eg
r e s si
o n 99
4 8
Sit
e 4 -T
otal P h
o sp h
o r u sSt
o rm L
o ad R
eg
r e s si
o n 1004 9
Sit
e 4 -C hl
ori d
eSt
o rm L
o ad R
eL I S T O F A B B R E V I A T I O N S
B
M
P
-B
e stM
a n ag
em
e ntP
r a cti
ceB O
D -B i
o ch
em i
c al O
xy g
e n D em
a nd
C
I -Ch l
ori
deC O
D -C h
e
m i
c al O
xyg
e nD
em
a nd
D E
M
-D iv
i
sio n
of
En vir o n
m
e nt al
M
a n ag
em
e nt(
N
o rth C
a r ol i
n a)
D
O
-D i
s s olv e
d Ox
y ge n
E
M
C
-E
v e ntM
e a nC
o nc entr ati
onE
PA
-E
n v
ir o n
m
e ntal
Pr ote ctio n
A g
e n cyG I S
-G
e og
r ap hi
cI
nf
o rm
ati
o nSy
s tem
M
SL
-M
e a nSe
a L e v el
N
P DE S
-N
ati
on al P
ollu
ti
o nD i
s ch
a rg
e El i m i
n ati
o nS
ystem
N U R
P -N
ati
on
w i d
eU
rb
a nR
u n of f P
r og
r am
P
O
TW
-P
u
b l i
cl
yO w
n ed T
r e atm
e ntW
o rk
sR C D
-R
e s o u r c eC
o n s e r v ati
o nD i
stri
ctS C S
-So
i l C
o n s e r v ati
onSe r v
i
ceS O C
-S
ynt
h
eticO
rg
a nic
C
om
po u nd
sT
DS
-T
ota
l D is s o
lv e
d So
l i d
sT S S
-T
o tal Su s
pe n
d
ed S
ol i d
sU N C
-U
ni
ver si
ty
of N
o rth C
a rol i
n a atC h
ap
el H il l
U SG S
-U
ni
t ed St
atesG
eolo
T h is
p
r oj
e ctw
a sm
ad
ep
o s sib l
e thr o ug h f
u nd i
ng fr om
th
eU N C D
epa r tm
e nt of
H
e al
th
a nd S
af
etyF i
rs t,I w
ould li k
e to th
a nk m y
res e a r ch
ad
vi
sor,D
rD
o n al d
EF
r a n ci
s c o,f
o rh i
sh
elp f
ul
e n c o u r ag
em
e nt a nd
c o n sta ntw i l l i
n
g
n e s s top
r o vi d
ea s sista nce t
h
r o ugh
o ut th i
sp
r oj
e ctI
am i
nd
eb
ted
t o D rF
r a n ci
s c of
o r th
e op
po rtu ni
tyto c o n
d
u ct r e s e a r ch i
nhi
s lab
or ato ry Iw
o ul d
al
s ol i k
e to th
a nk D
r Do n al d G
Wi l l h
oi
t a nd
D rS
tep h
e nC
W
h
al
e nf
o r th
ei
r ti m
ei
n r e vi
ew i
ng
thi
s r ep
o rtI
am
e sp
e ci
al l
yg
r atef
ul
tom
yf
am i l
yf
o r th
ei
r e nd l
e s sl
o v e, u nd
e rs tandi
ng
, a nd
su p po rt.
I w
o ul d
al
sol ik
e t o th
a nk m
yf
ri
e nd
si
n th
eC h
ap
el H i l l E
ngi
n e e ri
ng
D
ep
a rtm
e ntf
o r th
ei
r a s si
sta nce a nd
c am
a r ad
e ri
e Fi
n al l y
,
I w
ou
l d l i k
e to th
a nk
al l
of
m
yf
ri
e nd
s(
to om
a ny tom
e nti
o ni
nd i
vi d
u al l
y)
f
o r th
ed i
v e r si
o n s,f
u n, a nd
spe ci
al
ti m
e sA
.H
isto ry of the
C
r e ek a n dW
ate r shed
M
e etin
g
of
th
eW
ate rsCr e e
k h
a slo n
g b
e e n a n am
e ni
ty
a nd f
o c al p
oin
t of
th
eU
ni
v e r sit
y of N
o rth C
ar ol i
n a atC h
ap
el H il l
(
U N C
)
c am p
u s and
th
eN
o r th Ca r olin a
B ota nic a
l G
a rd
e n sW
h
e r e the
C
a r ol i
n a In n n ow
s ta nd
s,
w
as a"
s
p ri
ng
of
c o n si d
e r ab le
s
i
z e,k
n ow
n a s th
eC h
ap
el Sp ri
ng
,fr
om w hi
ch fl
ow
ed
the s tr eam w h i
ch w i
nd
si
tsw
ay
t
hr o u
g h p i
ctu r e sq
u e s c e nery
,
b y
th
eM
e etin
g
of
th
e
W
ate rstoM
org
a n 'sC
r e ek
"(
H
e nd
e r s o n, 1 9 4 9)
H i
stori
c al l
y, the c r e ek
a nd i
ts s u r r o u ndi
ng
path
s a nd
n atu r al
l
a nd
s c apeh
a v eb
e e n u s ed f
o r r e c r e atio n
,p i
c ni
c s, a nd
aq
uie
t e s c ap
efr
om
c am p
usli f
e(
Wi l
s o n, 195 3)
Rob
e rtH
o u se, aU N C
al
um
n u s(
1 9 12
- 1 9 1 6
)
a nd f
o rm
e rC h
a n c el l
o r,n ote
d i
nh i
sm
em
oir s
th
at th is
"w i l d
a r e af
o r stud
y a nd
r e c r e atio n
w
a s o nl
y afe
w
step
sfr
om
th
e cam p
u s a nd
vi l la
g
e"(
H
o u se,19 64
)
M
e etin
g
of
th
eW
ate r sC
r e ek h
a sb
e e n a nim p
o rta nt r e s o u r c e to th
eU N C
c o
m m
u nit
y Re s e a r ch
e r s,f
a c ult
y, a nd
stud
e ntsh
a v efr
eq
u e nted
th
e c r e ek
to c ol l
e cta n
d
stud
y aq
u ati
c o rg
a ni
sm
s a nd ri
pari
a n pla n
t spe ci
e sT h
eh
e ad w
ate r s of
th
e c r e ek
atC
ok
e rW
o od
sha s a
ls o
b
e e n uti l iz e
d
a s a con venie n
t "l i
vin
g
cl
as sr o om
"f
or a n um b
e r of
s cie n c e c
l
a s s e s.H
o u s e(
196 4)
r e c o u nted
vi
sit
s to th
e c r e ek
a nd it
ss u r r o u n
d in
gw
o od
sf
o rg
e og
r ap hy
a nd b i
olo
g y l
e sso nsw it
h D
r B a ttl
e a nd
Prof
es so rC
ol i
e rC
ob b
, z o olo
gy
le s s o n s
w it
h D
rH V
W
i l
son, and b
otany
cl
ass e sw i
th D
rW
C
C
ok
e r T od
ay, th
e sit
e of C
ok
e rW
o od
si
ssti l l
uti l iz e
d f
o r edu c a
ti
o n a nd
s ci
e nti fi
cr e s e a r c
h
(
D
eSa
ix
, 1 9 9 4
)
A
s theU
niv e r s
it
yh
a sg
r ow
n a nd d
e v elo
ped
, the c r e ek
a nd it
sw
at er sh
ed
ha v ec
h
a ng
ed d
r am
ati
c all
y L a nd
th
atw
as on c ed
omi
n ated b
yf
o r e sts a nd
ste ep r a vi
n e s,h
a sT
h
eh
e adw
ate r s of a n atu r al me a nd
e ring c r e ek
ha v eb
e e n tr a n sf
o rm
ed
to ad
e epl
yb
uri
ed
n etw
o rk
of
s to rm w
a te r c o n v eya n c e pi
pe sT h
e s e typ
e s of l
a nd
u s e ch
ang
e s are ty pic a
l of
a gr ow in
g u niv e r s
ity o r c om m
u ni
ty Th
ei m
pa cts of
th is
d
e v elo
pm
e nt,h
ow
e v e r, c a nb
e s e v e r e tob
oth
th
e qu a ntit
y a nd
qu al it
y of
str e am fl
ow
Ev e n
i
n 1 9 6 4,H
o u s e e xpr e s s ed
c o n c e r nf
o r th
e c r e ek
he had
e nj
oyed
a s a stu de nt "Th
e tr e e sm
e ntio n e
d b
y D r B at tle a r e
g
o n e, a nd
th
e sp
ri
ngsh
a v e eith
e rb
e e n in c o rpo r ated in thed
r ain age system
ofCh
apelH
i l l o r have dried upb
e c a u s e thetrees
h
a v eb
e e n r em
o v ed
.I
tis
j
u st a sw
el l
ab
o ut th
e sp ri
ng
sb
e c a u s e th
ew
at ers ar e n ol
o ng
e rd ri
nk
ab l
eE
v e n thef
ou ntai
n at th
eO l d
W
ell
on th
e cam p
u sg i
v es ci
ty w
ater,c o o
l
ed b
y r u n ni
ng
th
ep ip
ed
ow
ni
nto the
w
ate r s of
th
ew
ell
C i
vi l iz a
tio n pr e s e nts a c ons ta ntp
rob l
em
of
c o ntam i
n ated w
ate r"(
H
o u s e, 1 96
4)
B.
C
ha r a cte rist ic s of t heN
atu r alW
ate r shedT h
ew
ate rq
ual i
ty
of
a n atu ral
str e am i
s ch
a r a cteri
z ed b y l
o c al
cl i m
ate,to
p
og
r ap hy
,g
e olo
g
y, s oil
ty p
e s, a nd
str e am fl
ow
C ha
p
el H i l l
a nd U N C
a r el
ocated i
nO
r a ngeC
o u nty, a n a r e a c e ntr al l
yl
o c ated in
N
o rth C
a r oli
n a'
s
P i
ed m
o ntR
eg i
o n(
F i g
u r e 1)
T h
ew
ate r sh
ed
pr ed
om in a n
tlyd
r ain s
the
U N C
c am p
u s,lo c a
ted i
n th
e s o uth
e r np
orti
o n of C h
apel H i
ll
(
A
pp
e nd ix
1-M
ap
1)
Th
el
o c al
cl im
ate is cha r a cteri
z ed b
ym i l d w i
nte r s a nd h
ot,h
um i d
sum m
e r s Pr e ci p i
tatio ni
sg
e n e r al lyg
r e ate stdu
ri
ng
th
e■r^
1
—
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U
S B O R O•
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CH A RLO T T E
WIL M IN GT O N
S late A«;ricultu cal Experi me n t S ta tio n at Ralei g h
S tatio n : C H A P E L H I L L 2
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ID: 1 6 7 7S tate: NOR TH C A R O L IN A Co unt y: O R A N G E
Lati tude : 3 5:55:0 0 Long itude : 0 7 9:0 6:0 0
E le v a tio n: 5 0 0.0 0
Pa ramete r S tat is tic S. Yr E. Yr # Yr s # O bs % A
v g Ma x M in
AIR T E M P F A H N A I R TEM P F A H N EV A P TOT DA Y I N P R E C I P T O T D A Y I N S N OWD E P T H I N C H E S
M ini mum 194S 1 9 94 47 16 606 9 7 46 4 2 7 Maximum 19 4 8 19 9 4 4 7 16 67 8 9 7 7 0 6 5 9 Sum 1 9 4 8 19 9 4 47 1 2 1 7 9 71 55 73 3 Sum 1 948 19 94 4 7 1 6 7 6 2 9 8 4 5 49 7 Sum 1 9 4 8 19 9 4 4 7 1 647 3 9 6 4 6 2
5 118 1 4 18 5 7 4 7 0 7 6 8 10 4 5 7 4 5 5 3 0 3 5 7 8 8 3 3 3
2 5 1 0
From N CDC:Cl ima te D ata Ea st, 19 9 5
T he
w
ate r sh
ed
of
M
e etin
g
of
theW
ate rsC
r e eki
shi ll
y
,w it
h m
od
e r ate tos e v e r e s
l
op
e s, e sp
e cia
l l
yi
n th
e mi d d l
e r e a ch
e s
T h
e up p
e rp
a rt of
theb
a sin
h
a s am
axi m
um
el
e v atio n
of
ov e r50 0 f
e et me a n s e al
e v el
(
M
SL
)
T h
eU N C
mai
n c am p
u sis
s
i
tu ated
o n ag
e ntl
y sl
op i
ng
ri d g
e.D
ow
n str e am
of So u
th Ro ad
, the el
e v atio ndr
op
s sha r
pl
yb
ef
o r e e v e ntu al l
yfl
at te ni
ng
at th
eN C B
ota ni
c al G
a rd
e n sT h
ehi l l
yto
p
og
r ap hy
of
th
ew
ate r sh
ed
c o ntr ols s u r
f
a c edr a
in a
g
e a nd
aff
e ctsp
e r c ola
tio n
r ate s T heh
ydr a u
li
cl
e ng
th
of
th
ew
ate r sh
ed
, whi
ch
e x te nd
sfr
om
thefa r
th
e st poin
tin
th
eup pe r
b
a sin
to th
e c o nfl
u e n c e atM
o rg
a nC
r e ek
,is a
p p
r o xi m
atel
y 2 2m i
le slo n
g
.O
v e r th is
di
sta n c e th
ew
ate r sh
ed
el
e v atio n
d
r opsfr
om
r o ug hl
y52 0
f
e et to 2 5 0f
e et atM
o rg
a nCr e e
k
T h
e n atu r al w
ate rq
u alit
y cha r a c
te ris
ti
cs of
a str e am
a r e to s om
ed
eg
r e ed
ep
e nd
e nt o ng
e ol
og
yL
oti
c sys tem
s, su ch
a s a c r e ek
, a r em i
xtu r e s of g
r ou nd w
ate r ,d ir e c
t pr e ci
pit
ati
on, ov e rla n
d
r u noff
, a nd di
s ch
a rg
ew
ate rsT h
e ch
em i
c al
si m i la r roc
k
ty p
esi
nfl
u e ncin
g
th
eg
rou ndw
ater ch
em i
stry
a nd
c ons eq
u e ntly p
r odu
c e sgr o u n
dw
ate r of
si m i l
a rq
u al i
ty(
F i
gu r e 2)
M
e eti
ng
of
th
eW
ate r sC
r e ek i
slo c a
ted in
th
e up p
e rC
ap
e Fe a r Riv e r
b
a si
nw it
h i
nG
e o ch
em ic a
l Z
o n e I I(
Fi g
u r e 2)
T hi
s z o n eis u n
d
e rla
in
b
ym
etam
o rp h
o s ed
v olc a n
i
c a nd
s ed i m
e nta ry r o ck
s th
at a r em
od
e ra tel
y s olu
b l
e.T h
e s ol
ub i li
typ
r od
u c e sm i
n e r al i
z ed
gr o u nd w
ate r sw i
th
ty
pi
c al d i
s s olv ed
s ol i d
s c o n c e ntr ati
o n s r a ngi
ng fr
om
2 0to 6 0
m
g/ 1
(
C
r aw f
o rd
, 1 9 8 5)
T
h
e o v e rb
u rd
e n s oi l
si
n th
ew
ate r sh
ed
c o n sist of
upl
a nd m
ate ri
als
th
a tw
e ath
e r ed m
ai
nl
yfr
om
gr a ni
te a nd g
n eis s
(
U SD A
, 1 9 7 7)
Fr om fi
el d w
o rk
c om p l
eted
b
etw
e e n 1 9 7 0 a nd
1 9 7 5, th
eSo
i l C
o n s e r v atio n
S
e r v
i
c e(
S C S
)
cl
a s si fi
ed
s oi l
sin
th
ew
ate r sh
ed
a sp
r ed
om i
n a ntl
y of
the
A p p l i
ng
-H
ele n a
A
s s o cia
tio n(
U SD A
,
19 7
7)
T hi
s ass o ci
atio n
i
s ch
a r a cte riz e
d b
y "g
e ntl
y sl
op i
ng
and
slo
p i
ng
,
w
el l dr a
i
n ed
a nd
m
od
e r atel
yw
el l dr a
i
n ed
s oi l
s thath
a v e a s u rf
a c ela
ye r of
s a ndy l
o am
a nd
a sub
s oi l
of
s a n
d
y cla
yl
o am
, cla
y, o r s a nd
y cla
y ; o n up l
a nd
s "(
U SD A
, 1 97
7)
SC S
r ep
orts th
atth
is a s s o c
i
ati
o nha s
p
ote ntia
l f
o r c r ops,f
o rm
o st u rb
a n u s e s, a nd f
o r u s e a sw
o odl
a nd
sT h
r e e s oil
s e ri
e sd
om i
n ate th
ew
ater sh
ed
a nd
c om p
ri
se r o ug hl
y o n e thi
rd
of
th
ea r e a e a c
h
(
Fi
gu r e 3)
;W
ed
ow
e e s a nd
yl
o am
o n15
%
to 2 5%
slo
pe s(
Wm E
)
,A
p pl i
ng
-U
rb
anl
a nd
com p l
ex o n 2%
to 10% slo
p
e s(
A
uC
)
, a nd U
rb
a nl
and
(
U
r)
T h
eA p p li
ng
-U
rb
a nl
a nd
c om
pl
exis
ab
o ut2
5 to5
0 pe r c e ntA
pp l i
ng
s oi l
s a nd
2 0 to 4 0 pe r c e ntu r
b
a nl
a nd
(
U SD A
, 19
77
)
T hi
s s oi l
s e rie s
ch
a r a cte riz e
sa r e asth
ath
a vel ik
el
yb
e e nm
od i fi
ed w i
th fi l l m
ate ri
al
,
g
r ad
ed
,p
a v ed,
o rh
ad m
u ch
of
th
e o ri g i
n al
s oi l
rem
o v ed b
y c o n str u cti
o n a ctivit
ie s
(
U SD
A
, 1 9 7 7) W
ed
ow
e e s a nd
yl
o am
s oi l
s a r eg
e n e r al l
y o n si d
e sl
ope s ad
j
a c e nt tod
r ain ag
ew
ays a nd
s upp
o rtm
o stl
yw
o od l
a nd
s In th
eW
ed
ow
e e s oi l
a r e a s, slo
p
e a nd l
ow
tom
od
e r atep
e rm
e ab i l i
t yin
c r e a s e them
ag
nit
ud
eo
f
s oil
e r o sio n
a nd
s u rf
a c e r u n off
U
rb
a nla n
d
(
U
r)
c o n si
sts of
a r e a s th
at al
te r o v e r 8 0 pe r c e nt of
the n atu r al s oi l i
n th
ep
r o c e s s of
u rb
a niz a
tio n(
U
SD A
, 1 9 7 7)
A
s aU
t :
o ^ 4-1
o t / )
<u c
o
N
1 3
u
E
4 ) CJ O (UO
(U a n i
n
V
190 MIUS
ISO K IL O M EURS
EX PLA N AT I ON
"
TT
Ceoche tnieol l one fy ^ Copi Fjof R i»«r bo sinO
Study S i lc Lo c al io nW mO
m
m
W m£
m
D
uri
ng
a sto rm
ev e nt, s oi l
pr o pe r ti
e si
nfl
u e n c e th
em
agni
tud
e of
s u rf
ac e r u n of f
B a s ed
o n th
e s e pr ope rti
e s, e a c
h
s oi l
s eri
e si
s c ategori
z ed b
ySC S i
nto o n e of f
o u rh
yd
r ol
o gi
c s oi l g
r o upsT h
eA
p pl i
ng s oi l
s eri
e si
sd
efi
n ed
a s gr o up
B s oil
s th
at a r em
od
e r atel
yd
e ep
a nd w
el l d
r ai
n ed
(M
o ck
u s,
19
7 2)
U
rb
a nl
a nd
s oi l
s a r ed
efi
n ed
ash
yd
r ol
og i
cg
r oup C
a nd p
r od
u c em
o r e r u n of f
th
a n gr o up
B s oi l
s Th
e gr o up C
s oil
sh
a v e sl
ow i
nfi l
tr ati
o n r ate s a nd
c o ntai
n al
ay
e r th
ati m p
ed
esd
ow
nw
a rd m
o vem
e nt(M
ock
u s, 1 9 7 2
)
Th
eW
ed
ow
e e s a nd
y lo am
s eri
e s a r el
o c ate
d
o n slope s ad
j
a c e nt to th
e c r e ek
T h i
s s eri
e si
sd
efi
n ed
a s gr o up D a nd i
s ch
a r a cte ri
z ed b
yhi
gh
r u n of f
p
ote nti
al
, s
h
al l
ow
cl
ay s oi l
s, a nd
ah i g h w
ate r tab l
e(M
o ck
u s, 1 9 7 2
)
C
.T
heR
e s e a r chS
tud
yB
ef
o re th
ew
ate r sh
ed
of
M
e eti
ng
of
th
eW
ate r sC
r e ek b
e cam
e e xte nsi
v el y
d
e v el
op
ed
, th
e c r e ek m
ai
nta
i
n ed
th
e ch
a r a cteri
sti
c s of
a n atu r al
str e am
T h
eg
r ow
th
of
th
eU N C
c am p
u sh
a s c o n v e rted
th
ew
ate r sh
ed l
a nd
u s ef
r om m
o stl
yf
o r e sted
topr e
d
om
in a ntl
yi
n sti
tutio n al l
a nd w i
th
s om
e r e sid
e nti
al
a r e a s Thi
s ch
a ngei
nl
a nd
u s eh
a sh
ad
pr of
ou nd
ef f
e cts o n th
e c reek
a nd
th
e o rg
a ni
sm
si
t s up
port s Fo rm
a ny ye a r sn o
w
,
m
em b
e r s of
th
e c am
pu s c om m
u ni
ty a nd
vi
si
to r s t o th
eB
ot ani
c al G
a rd
e n sh
a v e r epo rt ed w
ate rd i
s c ol
o r ati
o n a nd m
aj
o r a e sth
eti
c pr ob l
em
sw i
th
th
e c r e ek
(
M
cC
o rm i
ck, 1 9 9 4)
Bef
o r e thi
s stud
y,fi
sh
,f
r og
s a nd
o th
e r aq
u ati
c o rg
a ni
sm
sw
e r eb
e com i
ng
s c a r c e o rw
e re n ol
ong
e rp
r e s e nt, e sp
e ci
al l
yi
n th
e up
str e am
r e a ch
e sT hi
sr e s e a r c
h p
r oj
e ctw
a s th
e r ef
o r ei
ni
ti
ated
to ad d
r e s sw
ate r sh
ed d
e v el
op m
e nti m p
a cts ,p
ol l
u ti
o n s o u r c e s, a n
d
th
ed
eg
r e e of w
ate rq
u al i
tyi m p
ai
rm
e nt atM
e eti
ng
of
th
eA
.R
egu lati
n gW
ate rQ
u al i t yO
v e r th
ela s
t tw
od
e c ad
e s, r e s e a r ch
ef fo
rts a c r o s s th
e c o u ntr
y h
a v edi
s c o v e r ed
m
a ny of
th
ed
eg
r ad i
ng i m p
a cts u rb
a niz a
ti
o n c a nh
a v e on r e c ei
vin
g w
ate rsD i ff
e r e ntl
e v el
s of g
o v e r nm
e nt a r e r e sp
o n si b l
ef
o r r eg
ul
ati
ng
the
a sp
e cts of f l
oodi
ng
,
s e
d i m
e ntati
o n, a nd w
ate r qu al i
ty
pr ob le
m
s InN
o rth C
a r ol i
n a,"
f l
o odi
ng i
s ad d
r e s s ed
pr
i m
ari l
y at th
el
o c al
a nd fe
de r a
l le v e
l
s, s ed i m
e ntati
o n at th
e state a nd l
o c al le v e
ls a n
d
i
nf
eri
o rw
ate rq
u al i
t y at th
ef
ed
er al
a nd
statel
e v els
"(M
al
c om
, 1 983
)
.Fe
d
e r al
r egula
ti
o n s,in c
lu
d i
ng th
e F ed
e r al
W
ate r Pol lu
ti
o nC
o ntr ol A
ct(
c om m
o nl
y r ef
e r r ed
to a s th
eC l
e a nW
ate rA
ct)
,w
e r efi
r st e stab li
sh
ed
to ad d
r e s s th
ep
ollu
ti
o nfi
-o
m p
oi
nt s o u r c e s, su ch
a si
nd
u stri
al
a nd m
u ni
ci p
al w
a stew
ate rd i
s ch
a rg
e s(
L
udw i
szew
sk i
,19 9 5
)
C
o ng
r e s sd
e cla r e
d
th
at the
ob
j
e cti
v e of
th
e 19 7
2 a ctw
as"
to
r e sto r e a n
d m
ain
tain
th
e ch
emi
c al
,p h
ysic a
l
a nd b i
olo
g i
c al in
tegri
ty of
th
eN
ati
o n 's
w
ate r s"(
A d l
e r, et al
, 19
9 3)
B
e si d
e s r eq
ui ri
ng p
e rm i
tsf
o r all p
oin
t s o u r c edi
s ch
a rg
e s, th
e a ct r eq
uir e
d
state s tod
e v el
opw
ate r qu ali
ty sta nd
a rd
s a nd
toi d
e nti f
y al l
w
ate r s n otm
e etin
g
th
e s e sta nd
a rd
sA d di
ti
o n al p
ollu
ta nt r ed
u cti
o n s n e c e s s a ry toa c
h i
ev e th
e s e sta nd
ard
sw
e r e th
e n t ob
ein c
orp
ora ted i
nto th
ep
e rm i
t r eq
uir e
m
ents Ev e ni
n 1 9 7 2,h
ow
e v e r,C
ong
r es s r e cog
ni
z ed
th
at th
eN
ati
on'
s
w
ate rsw
ere al
s ob
ei
ng d
eg
r ad
ed b y d if f
u s e,n o n
p
oi
nt s o u r c e s of p
ol l
utio n
Se
c ti
o n 2 0 8 of
th
e a ct requir ed
state s toi d
e nti
fy
all
s o u r c e s of
pol lu
tio n a nd
tod
e v elop a c om
pr ehe n si
v ew
ate rq
u al i
typ l
a n nin
g
a nd
ma n ag
em
e ntp
r og
r am
(
Ad le r
, et al
, 1 9 9 3)
Thi
sw
ate rshe
d
ap pr o a c
h w
a sla r
gel
y ab
a nd
o n ed b
y E PA
a nd
th
e state sin
th
e 1 9 8 0'
s,
b
utha s s
in c e
T
h
eC l
e a nW
ate rA
ctw
a sm
od i fi
ed i
n 1 9 7 7 toi m
pr o v e th
e c o ntr ol
of
to xi
cc o
m
po u nd
s r el
e a s ed i
nto s ew
e r s a nd
s u rf
a c ew
ate r s(
A dl
e r, et al
, 1 9 9 3)
In 1 9 8 3, th
eU S
En vi
r o nm
e ntal
Pr ote cti
o nA
ge n cy(
E PA
)
r epo rted
th
e r e s ul
ts of
th
eN
ati
o nw i d
eU
rb
a n Ru n of F
Pr ogr am
(
N U R P
)
Thi
s stud
yi
nd i
c ated
th
at u rb
a n storm w
ate r r u n of f
w
a s am
aj
o r n o npoi
ntp
ol l
uta nt s o u r c e c o ntrib
uti
ng
to str e am d
eg
r ad
ati
o n Th
e ni
n1 9 8 7,
C
o ng
re s sp
ass ed
th
eW
ate rQ
u al i
ty A
ct t o add
r e s s n o np
oi
nt s o u r c e s of
po l
l
utio n, s u ch a s u rb
a n sto rm w
ate r a nd
agri
c ul
tu r al r u n oflf
Re c ognizing th
ew
ate rq
u al i
ty im p
a cts of
u rb
a ni
z ati
o n, s e cti
o n 4 0 2(
p
)
of
th
e a ctd i
r e cted
th
e E PA
to"
p
r om
ul g
ate r eg
ul
ati
o n s to r eq
ui
r eN
ati
o n al P
oll
uta ntD i
s ch
a rg
eE l i m i
n ati
o nSy
stem
(
N P D
ES
)
P
e rm i
tsf
o r s to rm w
ate rdi
s ch
a rg
e s"(
L i
nd
s ay,19
9 1)
.T h
ed i
s ch
a rg
e of
sto r
m w
ate r r u n of f fi
'o
m l
a rge u rb
a n a r e a s(
p
op
ul
ati
o n gr e ate r th
a n 1 0 0,0 0 0)
a nd
i
nd
u s tri
al
a r e a sw
a si
n af f
e ct n ow b
ei
ng
c o n si d
e r ed
ap
oi
nt s o u r c e of p
ol l
uti
onw i
th
s
i m i l
a r c o ntr ol
s a si
nd
us try
a nd w
as tew
ate r tr e atm
entp l
a ntsBe c a u s e
C h
apel H i l l
a nd
th
eU N C
c am p
u s tog
eth
e r a r e n ot c o n si d
e r ed
al
a rg
em
u ni
ci
pali
ty(p
opul
ati
o ni
sl
e s s th
a n 1 0 0,0 0 0)
, the Tow
n a nd U
ni
v e r si
ty a r e n otm
a nd
ated
tom
o ni
to r a nd
r egul
ate th
ei
r sto rm w
ate rd i
s ch
a rg
e sS m
al l
c om m
u ni
ti
e sc a n st
i l l d
eg
r ad
e a r e c ei
vi
ng w
ate r,h
ow
e v e r, and l
o c al
o rd i
n a n c e s s u ch
a sC h
ap
el
H i l l
's R e s o u r c e
C
o n s e r v ati
o nD i
stri
ct(
R C
D)
h
a v eb
e e n e stab l i
sh
ed
to c r e ate ri p
a ri
a nb
uf f
e r s a nd
t op
r ote ct str eam
sfi
om
th
ei m p
a cts of d
e v el
op m
e ntS
til l i
n19 8 8
, th
eE
P A r epo rt ed
toC
o ng
r e s s "th
atp
oll
uti
o nfi
-o
m d iff
u s e o r n o npoi
nt s o u r c e s s u ch
a sr u n o
f f f
r om
u rb
a n a r e as a nd i
nd
u strial
si
te sw
a s ci
ted
a s th
el
e ad i
ng
c a u s e of w
ate rq
u al i
tyi m
pai
rm
e nti
n 3 7 state s"(
U S
E PA
, 1 99 1
)
.B . T he I
m p
a cts of
a D e v elop in
g
W
ate r shed
T
h
ed
eg
r e e of i m
pa ct o n a n u rb
a n str e am i
s aS
a n cti
o n of
th
ei
nte n si
ty of
d
e v el
opm
e nt a nd
th
e am
o u nt of
a r e a c o n v e rted
toi m p
e r vi
o u s s u rf
a c e s(
r o ad
s,p
a rk i
ng
l
o ts,b
ui
ldi
ng
s, etc)
Th
e c o n v e r si
o nw i
thi
n aw
ate r sh
ed f
r om
n atu r al
v egetated l
a nd
toi
m
pervio u s su rfa c e s af fe cts str e am
h y dr olog y, ge om
o rp holog
y,w
ate r qu al ity, aqu aticc o
m p
a cted
a nd
r e su rf
a c ed w i
th im p
e r vi
o u sm
ate ri
al
s,l
e s s r ai
ni
s al l
ow
ed
toi
nfi l
tr atei
nto th
e s oi l
a nd
r e ch
a rge th
e gr o u nd w
ate rP
a rk i
ng l
ots, r o ad
s,b
uil d i
ngs, a nd
sto r
m w
ate r c o n v ey
a n c e s c r e ate sm
o oth
e rh
yd
r a ul i
c su rf
a c e s a nd d
e c r e a s e th
e ti m
e of
c o n c e ntr at
i
o n of
sto rm w
ate rfl
ow
s(
S
ch
u el
e r, 1 9 9 1)
C
o n s equ e ntl
y,m
o r e of
th
estr e a
m
's a n n u al fl
ow i
s c o ntri b
uted b
y sto rm w
ate r r u n of f
a nd l
e s si
s c o ntri b
uted b
yb
a s efl
ow g
r o u ndw
ate ri
np
uts(
F i g
u r e 4a)
T h i
s c r e ate s ah
yd
r ol
og i
c r eg i m
echa r a cteri z e
d b
yh i
gh
a nd fl
a sh
y sto rm fl
ow
sf
ol l
ow
ed b
y r ed
u c ed d
ry-w
e athe r fl ow
s(
F i
gu r e 4b
)
A
s aw
ate r sh
ed
c o nti
n u e s t ob
e c om
ed
e v el
op
ed
,m
or e a nd m
or e rai
nf
al l i
sc o n v e rte
d
to s u rf
a c e r u n of f
,i
n c r e a si
ng
th
e v ol
um
e a nd
v el
o ci
ty
of
sto rm fl
ow
s, th
epe a
k d i
s cha rge r ate, a nd
the s e v eri
ty a nd fi
equ e n cy of fl
o od i
ng e v e nts(
Fi
gu r e 4b
)
Ine xtr e
m
el
yd
e v el
oped w
ate r sh
ed
s(
gr e ate r th
a n 5 0p
e r c e nti m
pe r vi
o u s)
, th
ep
o std
e v el
op m
e ntp
e ak di
s ch
arg
e r atem
ayi
n c r e a s eb
y af
a cto r of fi
v efr
om
th
epr e
d
e v el
op m
e nt r ate(
S
ch
u el
e r, 1 9 9 1)
U
rb
a n str e am
ch
a im
el g
e om
etry ad
j
u sts t o th
eh
yd
r ol
og i
c al
ch
a ng
e s c a u s ed b
yd
e v el
op m
e nti
n th
ew
ate r sh
ed
I
n c r e a s ed
r u nof f
v ol
um
e s a nd
v el
o ci
ti
e s r esul
ti
nstr e a
m b
a nk
e ro si
on, ch
a n n el w i d
e ni
ng
, a nd i
n c r ea sed fl
o odp l
ai
n el
e v ati
o ns(
F ig
u r e 4c)
T
h i
sp
r o c e s s c a n c o nti
n u ef
o r 1 5, 3 0 o rm
o r e ye a r s u nti l
th
e str e am
r e e stabl i
sh
e s as ta
b l
e ch
a n n el g
e om
etry t o ac com m
od
ate th
e ad d i
ti
on al
r u n of f
(
W
i l
son, 19
8 3)
.A d
j
u stm
e nts toh
yd
r ol
og i
c a nd h
yd
r a ul i
c ch
a ng
e s al
soi
n c r e a s e s edi m
e ntl
o ad
s to th
ec r e e
k
In c r e a s ed
s ed i m
e ntl
o ad
si
n tu r n al
te r str e am m
o rp h
ol
og
y a nd
th
e n o rm
al
s u
b
strate of
th
e c r e ek b
ed
C h
a n n el
s ed i m
e nt s sh i fl
;fr
om
c o a rse-g
r ai
n ed p
a rti
cl
e sto
w
a rd
s am i
xtu r e of fi
n e a nd
c oa r s e-g
r ai
n ed p
a rti
cl
e s Th
e s a nd
, s
il
t, a nd
cl
ay
p
a rti
cl
e sfi l l
up th
ei
nte r sti
ti
al
v oi d
sb
etw
e e nl
a rg
e r c ob b l
e s a nd g
r a v el
si
n ap
r o c e s sc a
l l
ed im b
ed d i
ng(
S
ch
u el
e r, 19
8 7)
C
o n str u cti
o n a nd l
a nd d i
st urbi
ng
a cti
vi
ti
e s ca n c r e atem
a s si
v e s edi m
e ntl
oad
sa n
d
gr e atlyi
n c r e a s e tu rb i d
ityl
e v el
sd
uri
ng a sto rm
e v e ntO
n c e c o n str u cti
o ni
sc o
m
pl
eted
a nd
th
el
a nd i
s v eg
etated
a nd
stab il i
z ed
, th
ew
ate r qu al i
ty ef f
e cts of
u r