, 2166 m, 4162 m,,, 29 10 3 m 3 gs, 924 10 8 m 3,, 5 10, 7117%, 11 4, 2813%,, 266 10 3 m 3 gs, ;, ;,,,,,,,,



Σχετικά έγγραφα
GPS, 0. 5 kg ( In tegrated Fertility Index, IF I) 1. 1 SPSS 10. IF I =

hm 2,, , hm 2, A CTA GEO GRA PH ICA S IN ICA

G IS N N E E, , km 2, 92% A CTA GEO GRA PH ICA S IN ICA

V o l122, N o13 M ay, 2003 PRO GR ESS IN GEO GRA PH Y : (2003) , : TU 984. , (Eco logy fo r evil) [1 ] (R ich Boyer), 2.

V o l. 53, N o. 3 M ay, 1998 A CTA GEO GRA PH ICA S IN ICA ) m 3 gs,

, E, PRO GR ESS IN GEO GRA PH Y. V o l122, N o15 Sep t1, 2003 : (2003) , 263, (0 1m ) P93511; P42616

26 3 V o l. 26 N o A cta Eco logiae A n im alis Dom astici M ay ,

ED SS (Environm en tal D ecision Suppo rt

( , ,

ZrO 2, ZrO 2. (M ) W O 3g ( 100% ) SO 4 2- W O 3 M oo 3, SO ( Zr (OH ) 4 ) ( ( 0. 1 mo l. L - 1 A gno 3 ), Zr (OH ) 4 SO (0.

T he Op tim al L PM Po rtfo lio M odel of H arlow s and Its So lving M ethod

V ladim irov A CTA GEO GRA PH ICA S IN ICA China Academic Journal Electronic Publishing House. All rights reserved.

1998, 18 (1): 1 7. A cta T heriolog ica S inica (,, ) (Grow th layer group s, GL Gs) 168, 42,

Con struction and D emon stration of an Index System of Know ledge Amoun t of Po sition

Error ana lysis of P2wave non2hyperbolic m oveout veloc ity in layered media

A R, H ilbert2h uang T ran sfo rm and A R M odel

Im pact of capac ity a lloca tion on bullwh ip effect in supply cha in

Bank A ssetgl iab ility Sheet w ith Em bedded Op tion s

,,, (, ) , ;,,, ; -

(T rip tery g ium w ilf ord ii Hook) ,Beroza [6 ] 4 W ilfo rine W ilfo rdine W ilfo rgine W il2. Euon ine 1. 0% 1980, 1. 1 ; 1. 0%, ; 0.

China Academic Journal Electronic Publishing House. All rights reserved. O ct., 2005

Jou rnal of M athem atical Study

A CTA GEO GRA PH ICA S IN ICA

G IS A CTA GEO GRA PH ICA S IN ICA. V o l. 55, N o. 1 Jan., 2000 : (2000) E2m ail: lreis1ac1cn

(H ipp op hae rham noid es L. ) , ; SHB 2g , 1. 0, 2. 0, 3. 0, 4. 0, 5. 0 ml mm. : Y = X - 0.

U (x, y ) = : K (x i- x k) K (x i- x k, y j- y l), 2. 1

, 1, 3, 3. Stud ies on the In terspec if ic A ssoc iation of Canopy Trees in D avid ia

M athem aticalm odel and A lgo rithm of In telligen t T est Paper

6 cm, 1. 2 IAA, NAA, 2. 1

D EM, ], 1969 F reeze H arlan : SH E G IS Tsinghua Tongfang Optical Disc Co., Ltd. All rights reserved.

copula, 5 3 Copula Κ L = lim System s Engineering M ay., 2006 : (2006) ,,, copula Ξ A rch im edean copula (Joe,

) V o l. 40 N o. 6 : A : Q ,, W ard [ 1 ] (A v icenn ia m a rina) (K and elia cand el)

; (A con itum kusnez of f ii R eichb. ),.

, ( , (P anax qu inquef olius) ) ; L C2V P series U H PE), M Pa R E252. C18 (5 Λm, 250 mm 4. 6 mm ) ( )

Η βραχόπτωση της 17/12/09 στα Στενά των Τεµπών, σε σχέση µε τις δονήσεις των ανατινάξεων διάνοιξης της νέας οδικής Σήραγγας

, 4, 6, 8 m in; 30%, 50%, 70%, 90% 100% 15, 30, 45, 60, s V c

TR IBOLO GY N ov, 2004 , P I2. , 120 M Pa, P I. 6 mm 7 mm 30 mm [7, 8 ] mm,. JSM 25600LV 1. 1 (EDXA ).

: (2003)

O verlay A lgo rithm of H ierarch ical M ap s

, ( CO 2+ O 2+ N 2, ], N 2 [ 14, 15 ] O 2. ( 0. 1 ml ) ; (23 Jayasingh h atm ) (2001) [ 7 ]

Section 8.3 Trigonometric Equations

1, +,*+* + +-,, -*, * : Key words: global warming, snowfall, snowmelt, snow water equivalent. Ohmura,,**0,**

Main source: "Discrete-time systems and computer control" by Α. ΣΚΟΔΡΑΣ ΨΗΦΙΑΚΟΣ ΕΛΕΓΧΟΣ ΔΙΑΛΕΞΗ 4 ΔΙΑΦΑΝΕΙΑ 1

Approximation of distance between locations on earth given by latitude and longitude

D ecision2m ak ing M odel Inco rpo rating R isk Behavio r under P ro ject R isk M anagem en t

A CTA GEO GRA PH ICA S IN ICA

Phys460.nb Solution for the t-dependent Schrodinger s equation How did we find the solution? (not required)

«ΑΝΑΠΣΤΞΖ ΓΠ ΚΑΗ ΥΩΡΗΚΖ ΑΝΑΛΤΖ ΜΔΣΔΩΡΟΛΟΓΗΚΩΝ ΓΔΓΟΜΔΝΩΝ ΣΟΝ ΔΛΛΑΓΗΚΟ ΥΩΡΟ»

(TPP)Co 1. 1 ], [ 1, 2 ] V o l. 3 N o. 4 N ov EL ECTROCH EM ISTR Y ) ) ,, Co V V. (T PP) Co (Py) , - 1.

:,UV IKON 810, 700 nm. DU 27Spectropho to neter 1. 1 U S2KT P

ss rt çã r s t Pr r Pós r çã ê t çã st t t ê s 1 t s r s r s r s r q s t r r t çã r str ê t çã r t r r r t r s

ΑΡΙΣΤΟΤΕΛΕΙΟ ΠΑΝΕΠΙΣΤΗΜΙΟ ΘΕΣΣΑΛΟΝΙΚΗΣ ΤΜΗΜΑ ΟΔΟΝΤΙΑΤΡΙΚΗΣ ΕΡΓΑΣΤΗΡΙΟ ΟΔΟΝΤΙΚΗΣ ΚΑΙ ΑΝΩΤΕΡΑΣ ΠΡΟΣΘΕΤΙΚΗΣ

17 1 V o l. 17 N o CH IN ESE JOU RNAL O F COM PU TA T IONAL M ECHAN ICS February 2000 : A

( ) , ) , ; kg 1) 80 % kg. Vol. 28,No. 1 Jan.,2006 RESOURCES SCIENCE : (2006) ,2 ,,,, ; ;

Study on Re-adhesion control by monitoring excessive angular momentum in electric railway traction

Galatia SIL Keyboard Information

Comparison of Evapotranspiration between Indigenous Vegetation and Invading Vegetation in a Bog

Tsinghua Tongfang Optical Disc Co., Ltd. All rights reserved.

CHEM ICAL JOU RNAL O F CH IN ESE UN IV ERS IT IES [1, 2 ]. ., FT IR, , g ( cm - 1 ). H 2O cm - 1. :

On- l ine com puter detecting system of p ipel ine leak and its algor ithm


Research Progress of Collecting Ra in Effect in Urban Perv ious Surfaces

Rub isco. Rubisco. R ubisco R ubisco , R ubisco

,,,. , BM B 005 ( ] , SJM - IM L - 90 ( V ellank [ 15 ]

F ig. 1 Flow chart of comprehen sive design in the research of com patibil ity. E2m ail: ac. cn

Mean bond enthalpy Standard enthalpy of formation Bond N H N N N N H O O O

Resurvey of Possible Seismic Fissures in the Old-Edo River in Tokyo

Correction of chromatic aberration for human eyes with diffractive-refractive hybrid elements

Exercises 10. Find a fundamental matrix of the given system of equations. Also find the fundamental matrix Φ(t) satisfying Φ(0) = I. 1.

Boundary-Layer Flow over a Flat Plate Approximate Method

( ) ( t) ( 0) ( ) dw w. = = β. Then the solution of (1.1) is easily found to. wt = t+ t. We generalize this to the following nonlinear differential

Η ΕΡΕΥΝΑ ΤΗΣ ΓΛΩΣΣΙΚΗΣ ΑΛΛΑΓΗΣ ΣΤΑ ΚΕΙΜΕΝΑ ΤΗΣ ΜΕΣΑΙΩΝΙΚΗΣ ΕΛΛΗΝΙΚΗΣ: ΜΕΘΟΔΟΛΟΓΙΚΗ ΔΙΕΡΕΥΝΗΣΗ ΤΩΝ

Study on the Strengthen Method of Masonry Structure by Steel Truss for Collapse Prevention

Appendix. The solution begins with Eq. (2.15) from the text, which we repeat here for 1, (A.1)

ΟΙ ΕΠΙΠΤΩΣΕΙΣ ΤΗΣ ΑΣΤΙΚΟΠΟΙΗΣΗΣ ΣΤΑ ΥΠΟΓΕΙΑ ΝΕΡΑ ΤΗΣ ΕΥΡΥΤΕΡΗΣ ΠΕΡΙΟΧΗΣ ΠΕΡΑΙΑΣ, ΗΜΟΥ ΘΕΡΜΑΪΚΟΥ

A T H E R M A L M O D E L F O R T H E S U R F A C E T E M P E R A T U R E O F M A T E R I A L S O N T H E E A R T H 'S S U R F A C E

Το άτομο του Υδρογόνου

, , ; ,,, ,,, ; > cm , 62. 5% 66. 5%, 0. 2 g g,, 67% , , ;, , : V o l. 24, N o. 4 A ug.

IRBB 4 (Xa24) IRBB 7 (Xa27) IRBB 21 (Xa221) 6

UDZ Swirl diffuser. Product facts. Quick-selection. Swirl diffuser UDZ. Product code example:

Οι απόψεις και τα συμπεράσματα που περιέχονται σε αυτό το έγγραφο, εκφράζουν τον συγγραφέα και δεν πρέπει να ερμηνευτεί ότι αντιπροσωπεύουν τις

ΠΤΥΧΙΑΚΗ ΕΡΓΑΣΙΑ ΒΑΛΕΝΤΙΝΑ ΠΑΠΑΔΟΠΟΥΛΟΥ Α.Μ.: 09/061. Υπεύθυνος Καθηγητής: Σάββας Μακρίδης

ΔΙΠΛΩΜΑΤΙΚΗ ΕΡΓΑΣΙΑ ΕΠΑΝΑΣΧΕΔΙΑΣΜΟΣ ΓΡΑΜΜΗΣ ΣΥΝΑΡΜΟΛΟΓΗΣΗΣ ΜΕ ΧΡΗΣΗ ΕΡΓΑΛΕΙΩΝ ΛΙΤΗΣ ΠΑΡΑΓΩΓΗΣ REDESIGNING AN ASSEMBLY LINE WITH LEAN PRODUCTION TOOLS

Studies on the Athena Parthenos of Pheidias

Στέφανος ΧΑΡΑΛΑΜΠΟΥΣ 1, Ιωάννης ΚΑΛΟΓΕΡΑΣ 2, Ιωάννης ΣΤΡΑΤΑΚΟΣ 3, Μιχαήλ ΣΑΚΕΛΛΑΡΙΟΥ 4

, 300 # , 26. 7% g N ac l 0. 4 g KC l g CaC l2 2H 2O g N a2s 2H 2O g N ah 2PO 4. . P indbo rg [4 ],

ΥΩΡΟΘΔΣΖΖ ΚΑΣΑΛΛΖΛΩΝ ΘΔΔΩΝ ΔΓΚΑΣΑΣΑΖ Υ.Τ.Σ.Τ. ΜΔ ΣΖ ΥΡΖΖ G.I.S.: ΔΦΑΡΜΟΓΖ ΣΖ ΕΑΚΤΝΘΟ

1999, 17 (1): J ourna l of W uhan B otan ica l Resea rch ( ) ( ) 2, 3. (Celosia cristata L. ),

Retrieval of Seismic Data Recorded on Open-reel-type Magnetic Tapes (MT) by Using Existing Devices

ΚΛΙΜΑΤΟΛΟΓΙΑ CLIMATOLOGY

300071; 3. , ) E2m ail: 263. net CH EM ICAL JOU RNAL O F CH IN ESE UN IV ERS IT IES CH 2CO 2H N H H N

ΜΕΤΑΠΤΥΧΙΑΚΗ ΕΡΕΥΝΗΤΙΚΗ ΔΙΑΤΡΙΒΗ

A ( SPA ) Su lfo succin im idyl 62[ 3 2( 22pyridyldith io ) p rop ionam ido ]hexanoate (Su lfo2l C2SPD P) C E2m ail: w

«ΠΡΟΒΛΕΨΕΙ ΟΠΙΘΟΧΩΡΙΗ ΣΩΝ ΠΑΡΑΛΙΩΝ ΛΟΓΩ ΣΗ ΑΝΟΔΟΤ ΣΗ ΘΑΛΑΙΑ ΣΑΘΜΗ ΣΟ ΝΟΜΟ ΔΩΔΕΚΑΝΗΟΤ»

ΑΚΑ ΗΜΙΑ ΕΜΠΟΡΙΚΟΥ ΝΑΥΤΙΚΟΥ ΜΑΚΕ ΟΝΙΑΣ ΣΧΟΛΗ ΜΗΧΑΝΙΚΩΝ ΠΤΥΧΙΑΚΗ ΕΡΓΑΣΙΑ

Επίδραση της Συμβολαιακής Γεωργίας στην Χρηματοοικονομική Διοίκηση των Επιχειρήσεων Τροφίμων. Ιωάννης Γκανάς

R &D on Key T echno logies Based on W eb Info rm ation Pub lish ing System

D esign and Imp lem en tation of Parallel Genetic A lgo rithm

Fe, Cu, Zn,M n, Se I 54. 0, 9. 2, 11. 0, 66. 5, 0. 08, m ggkg, 100%, 200%, 300%

Research of Han Character Internal Codes Recognition Algorithm in the Multi2lingual Environment

Transcript:

55 2 2000 3 A CTA GEO GRA PH ICA S IN ICA V o l. 55, N o. 2 M ar., 2000 : 037525444 (2000) 0220243208 1, 1, 2 (11,, 200062; 21, 200002) :, 4,, 3,,,, : ; ; ; ; : P34315; P967 : A,, 80, 1, 2166 m, 4162 m,,, 29 10 3 m 3 gs, 924 10 8 m 3,, 5 10, 7117%, 11 4, 2813%,, 266 10 3 m 3 gs, 912, ;, ;,,,,,,,,, : 1999206202; : 1999210223 : (19492),, 1974, 20 E2m ail: h tshen@ sk lec1ecnu1edu1cn

244 55,,,,, 2 [ 1 ], 2 2,, 4 211 : (1),,,, ; (2),,, ; (3) 212,,,,,,,,,,, 1974 2 10 8 t [2 ], 1987 2 16 17, 148 10 4 t,,,,, :, ; (S4-5) (S6) (S7),, 1 (Clg 10-3 ) Ξ (198217) Tab11 Vertically averaged salin ity at the station s in the South and North Passage S4 S5 S6 S7 S1 S2 S3 0174 0136 0114 0105 0109 0116 0152 0144 0135 0112 0105 0107 0158 0137 1144 2104 0150 0133 0132 0167 1118 1139 1131 0165 0135 1115 1129 1154 Ξ :, ( ), 198819

2 : 245,,,,,,,,, ;,,,, ( 1) 1 a: S3 b: S5 F ig11 Changes of Ch lo rinity w ith velocity a: at ancho r station S3 in the N o rth passage b: at ancho r station S5 in the South passage 213 ( ),,,, ;,,,,, 214,,,,,,,,,,,

246 55,,, 3 311, 312 :, ;, ( 2) 2 F ig12 Curves of velocity and ch lo rinity during during tidal cycle a) b) a) influenced by saltw ater from N o rth B ranch b) uninfluenced by saltw ater from N o rth B ranch,,,, 3 :, ;, ;,, ;,, ( 3),,

2 : 247, 2019 10-3, 8185 10 23 6 10, 12 4,,,,, 100 10 26,,,, 50 10 26, 313 31311,,,, ;,,, 3 (19961318 29) F ig13 Sem imonth ly variations of ch lo rinity in the Changjiang estuary (19961318 29),, ( 2), 1996 3 11, 315 10-6 234 10-6 594 10-6, 279 10-6,, 2#, ;,,,,,,, 2#,,,, ( 3) ( 1978 1979 ), ( 1996 3 ),,,, 1996 3, 20 10 26 gkm, 70 10-6 gkm

248 55, 2 682 10-6,,,,,,,, 1, 1,,, 100 10-6 2 Ξ (Clg 10-6 ) Tab12 D istr ibution of chlor in ity along the South Channel-South Branch 198613111 12 62 67 160 261 198713115 16 157 182 291 788 19961317 38 52 Ξ Ξ 578 935 3 Ξ (Clg 10-6 ) Tab13 D istr ibution of the chlor in ity at station s in the south bank of Chong m ing island 2# 1996, 3, 8 ( ) 1242 400 837 1338 1996, 3, 13 ( ) 79 488 551 427 Ξ : Ξ Ξ., 1996. 31312, 3,, 50 10-6 ;,, 25%,, ; 3,,,,, 3,,, 250 10-6 4, 20 km, 200 10-6, 50 10-6,,,, 7215 km, 1156, 1 [3 ], 1985,, 13 10 6 m 3,, 200 10-6,, 200 10-6, :,.., 1981.

2 : 249 86 10 5 m 3,,, ( 250 10-6 ),,, 95% 97%,,, 20 km 8,, [4 ], 7,,,,, 217 913, 112 215,, 1987 31, 9 250 10-6,,,,,,,,,, [5 ], :,,,,,, 014 016,,,,,,, (References) [1 ] M ao Zh ichang, Shen H uanting. Study on type of saltw ater intrusion fo r tidal branch ing estuaries a case study on the Changjiang estuary [J ]. J ou rnal of E ast Ch ina N orm al U niversity, 1995 (3): 77 85. ( In Ch inese) [,. [J ]., 1995 (3): 77 85. ] [2 ] H an N aibin, L u Zhongyi. Study on the p rocesses and regulations of no rth branch in the Changjiang estuary[j ]. R enm in Changj iang, 1984 (3): 40 45. ( In Ch inese) [,. [J ]., 1984 (3): 40 45. ] [ 3 ] Shen H uanting, M ao Zh ichang, Gu Guozhuan et al. T he effect of South- to - N o rth w ater transfer on saltw ater intrusion in the,,.., 1996.

250 55 Changjiang estuary[a ]. In: Long- distance w ater transfer: a Chinese case study and international experiences[c ]. Published fo r the U nited N ations U niversity, 1983. 351 359. [4 ] H an N aibin. A nalysis of the ch lo rinity of South B ranch channel of the Changjiang estuary[j ]. J ou rnal of N anj ing H y d rau lic R esearch Institu te, 1983 (1): 74 81. ( In Ch inese) [. [J ]., 1983 (1): 74 81. ] [5 ] Shen H uanting, Yuan Zhendong, Zheng Yongbing et al. P rediction of how m any days it should no t be draw n w ater constantly from Yangtze R iver[j ]. M athem atics in p ractice and theory, 1997, 27 (3): 211 216. [J ]., 1997, 27 (3): 211 216. ] (in Ch inese) [,,. The Pattern of Saltwater In trud ing in to the Changj iang Estuary and the Utilization of Freshwater Resources M AO Zh i2chang 1, SH EN H uan2ting 1, XU Peng2ling 2 (11S tate K ey L aboratory of E stuarine and Coastal R esearch, Institu te of E stuarine and Coastal R esearch, E ast Ch ina N orm al U niversity, S hang hai 200062; 21S hang hai W ater W orks Corp oration, S hang hai 200002) Abstract: T he geom o rp h ic fea tu res of the Chang jiang estua ry a re cha racterized by the m u lti2o rder b ranch ing. T he saltw ater in tru sion has the fo llow ing fou r distinct fo rm s: d irect in t ru sion from the ou ter sea; sa ltw a ter exchange by shoa l p a ssages; sa ltw a ter dow n stream from o ther w aterw ays; saltw ater in tru sion by tidal flooding. T empo rtal changes in the salin ity of the Changjiang estuary have daily, sem imon th ly, seasonal and yearly variation. T here ex ists the sharp th ree dem arcation lines of salin ity gradien t along the Sou th B ranch- Sou th Channel. Tw o m ain p rob lem s had to be so lved befo re bu ilding reservo irs of avo ide saltw ater and sto re freshw ater in the Changjiang estuary. O ne is to calcu late the longest du ration that the ch lo rin ity exceeds 250 10 26 in the w ater resou rces area, w h ich is the criterion value fo r determ in ing the sto rage capacity of reservo irṡ M athem atical m ethods including the cybernetics, the frequecncy spected analysis and m athem atical modelling are adop ted here to get mo re co rrect tim es w hen the ch lo rin ity exceeds 250 10 26. A nd the o ther is to determ ine reasonab ly site of the pump ing station and the heigh t of w ater in take of w ater p um p s from the river bed. T he above p rob lem s can be so lved after understand ing the pattern of tempo ral and spatial variation of the saltw ater in tru sion in the Changjiang estua ry. T he above conclu sion s have p layed an impo rtan t ro le in fo rm ing the reservo ir schem e of the Bao shan lron and Steel P lan t, and supp lied basic data fo r selection of the po stion and sto rage capacity fo r the Chenhang reservo iṙ Key words: T idal b ranch ing estuaries; Pattern of salin ity vary w ith tim e and space; U tilization of freshw ater resou rces; R eservo irs of avo ide saltw ater and sto re freshw ater; Changjiang E stuary