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i <br /> IhWrolopV wIN hevs a drr�Mer pettem as bdoro the devNoPrt�t� in thet tM e�rly dormt dtw�dry <br /> perbd vrN esturate and AI up the wederd. Mr whxaHon.the weter wll weilbw�nd po tlraqh ths <br /> I culvsrl. Beaues moro w�ter hom a piven Morm wAI n�ch ths wMl�nd,M wN pob�bly rMch Mturtllon <br /> eomswfrt esrlbr In ths wet�eai.and thers wN bs rnore dbclrrps hom ths wNard. On averq�, <br /> tlnouph ths+wt seseo�the Iluctuetlon In wete►wIN bs ka end moro d the wMl�nd�N s�ed <br /> ( to be aturated. A hipher propdtlon d ths wetlend rrrY bscartb wkebls fa wetlend�p�cM�ad�pted <br /> fa seturated oaidkkvro (e.q• daqh eedpa, PadNc wllo�. At the end d ths wet ee�eon, ths ams <br /> proceee d drykq wiM feke plece. After developrnerK, however, there ia expected ro bs lea wate► <br /> I avaMeds In the suroundkp weterahed soll beceuse neerly heM the oripinel wets►ahsd wAI bs urWer <br /> pevert�ent. The reeUt Is expeated to be that the wedand vvNl reech ke Iete eurrwner dry etete eanewfrt <br /> eeAler. However. the wetland keelf may heve more wetx juat prbr to the dry eeeeon. The dNfe►ence <br /> I In drykp tkne mey Sc only dipht and heve no noticeeNe effect on the vepetatbn. Even N thers le an <br /> effect. N waAd p►obedy be manBest very elowly. <br /> I Q�y,�w. The ouMow irom Wetland B poee tMaph cilverts to the decenllon bealn on the Jolx� <br /> Fluke property. Thle Ilow wIN be rt�onMored uakq e wek end etaff pepe pleced In hont d ths ctAvert. <br /> A brddcrseted wek wN be wed In order nd to reetrlct the aAAow. Ths locetlon p►opoe�d M ths <br /> I �opoqraPMc MOh Pok�t thet detertnk�ee the devatlon d the wetx In the wedend� � h a iew feet <br /> Inelde the wetlerd hom the culvert opeM�p. The wek wAI be elzed to hendle the e�ected�tortn Ibw <br /> baeed on the modelMtp. <br /> I0►ourd wate►recl�arae. To complete the underelandlnp d the hydralopic repkne d Wetlend B, k <br /> wIN be neceemry to coNect IMametbrt on the eolle and pround-weter levele undeilykp the wetlend. <br /> � TMs kdartxtbn wIN provlde e means to determine the prou�d water Interactio�wkh the wetlend. le. <br /> whether water h laet to tha praxd throuph the beee d ths wedend. Beesd on INnked Hdd k�fartrrllon, <br /> the aseunption wae mede, for the purposee d modelkp end Nnpaq ae�seement. ttiet ths weWnd M <br /> l ��d�M by�„��ed, re�nre�y x�►�aa y�o�cn, x„dy��o cner�y inne wm�►�ai�►�d <br /> to tho praxd weter thraqn the beae d the wetlend. <br /> � In ordx to detertnine M encwgh water la beirp put inlo'' ,wedende to accouM hx netual toe�es <br /> ro the underlykp doep pround weter, k wAI be NnpoAent to determine rouphly how pertneaWs the <br /> � underlykq edl Is, en�l whether tho eeme eoA permeabAky occure throuflhari the wetlend. In addNlo�, <br /> the potenliel rate of inlptratlon losaea to the prauid weter wll be aaeeased beaed on observNq weter <br /> level dNferer�cea belween the wetlard end the aubeuAace. Tho eoN cheracterization end water levei <br /> iobaervatlons wNl be mede at e number d poiMs In the wedand uslnq heixlaupered eoN bork�ps. <br /> Sd eemplea wNl be cdlected hom the boreholee fa laboratory eneiysis d pemieebNlty. In eddkion, <br /> � elmple, emelltllemeter plezort�etero can be inatelled In eelected borelwles ro mo�lta the yround water <br /> level. <br /> The surfece-and pround-water monftping �xopram wNl ahow the Inteprated eMecte d water N�piR <br /> and output, indudinp ground water recherge end evapotraneplratlon This Informetbn wYl be Miportant <br /> In meki�p declsiona about(uAher manlpu�aqon d the wetland, eMher as continpency meawree or}or <br /> IenhancertierK opportunftles. <br /> Ir.�MA.�1��1�.��.Y W <br /> � DAME9 A MOORF <br />