List of Hydrological Stations Operating in the Ca River Basin

37



Figure 2.1: Map of hydrometeorological station network in Ca River basin


Currently, there are 16 hydrological stations in the basin (Table 2.2 ) including:

+ 08 level I hydrological stations: My Ly, Quy Chau, Nghia Khanh, Muong Xen, Dua, Yen Thuong, Hoa Duyet and Son Diem; measurement factors are water level, rainfall, flow, alluvium. My Ly hydrological station is a dedicated station located in the upper reaches of Nam Non river, serving the operation of Ban Ve reservoir.

+ 05 level III hydrological stations in river areas not affected by tides: Thach Giam, Con Cuong, Do Luong, Nam Dan, Chu Le; measurement factors are water level and rainfall.

+ 04 level III hydrological stations in tidal river areas: Cho Trang, Ben Thuy, Cua Hoi, Linh Cam. Ben Thuy station is managed by the Department of Agriculture and Rural Development of Nghe An province.

Table 2.2: List of hydrological stations operating in the Ca River basin


TT

Station name

Basin

river

Coordinates

Important factors

measurement

Five years

measurement

1

My Ly

Chief

19°37'59'' - 104°18'48''

X, H, Q

2010 - present

2

Muong Xen

Tomb

19°24'17'' - 104°08'25''

X, H, Q, T

1969 - present

3

Stone Temple

Chief

19°15'54'' - 104°28'00''

X, H, T

1959 - present

4

Con Cuong

-

19°02'49'' - 104°53'17''

X, H, T

1962 - present

5

Quy Chau

Filial

19°33'07'' - 105°05'45''

X, H, Q, ρ, T

1961 - present

6

Nghia Khanh

-

19°12'22'' - 105°23'35''

X, H, Q, ρ, T

1969 - present

7

Coconut

Chief

18°59'15'' - 105°02'43''

X, H, Q, ρ, T

1959 - present

8

Do Luong

-

18°54'48'' - 105°17'57''

X, H, T

1962 - present

9

Yen Thuong

-

18°41'14'' - 105°26'22''

X, H, Q, ρ, T

1968 - present

10

Nam Dan

-

18°41'47'' - 105°29'46''

X, H, T

1962 - present

11

Zhou Li

Thousand Deep

18°10'55'' - 105°42'05''

X, H, T

1974 - present

12

Hoa Duyet

-

18°23'08'' - 105°35'57''

X, H, Q, ρ, T

1959 - present

12

Son Diem

Thousand Streets

18°30'25'' - 105°21'55''

X, H, Q, ρ, T

1961 - present

13

Intuition

La

18°31'35'' - 105°33'18''

X, H, T

1963 - present

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TT

Station name

Basin

river

Coordinates

Important factors

measurement

Five years

measurement

14

Trang Market

Chief

18°34'50'' - 105°38'49''

X, H, T

1962 - present

15

Ben Thuy

-

18°39'03” - 105°42'30"

X, H, T

1960 - present

16

Hoi Gate

-

18°44'59'' - 105°44'13''

X, H, T

1965 - present

Note : H: water level, Q: flow, ρ: sediment

The entire basin has 9 rain gauge stations (Table 2.3 ). Since 2018, these rain gauge stations have been upgraded to automatic rain gauge stations.

Table 2.3: List of rain gauge stations in the Ca River basin


TT

Station name

Coordinates

Element

monitoring

Five years

measurement

1

Que Phong

19°36'29'' - 104°55'23''

X

2008 - present

2

Farm 3/2

19°21'59" - 05°16'59"

X

1960 - present

3

Farm 1/5

19°22'59" - 105°29'59"

X

1960 - present

4

Dong Hieu

19°18'0.2" - 105°29'59"

X

1960 - present

5

Leaf Slot

19° 05'00" - 105°19'59"

X

1958 - present

6

Khe Bo

19°10'53" - 104°39'55"

X

1960 - present

7

Salt Waterfall

19° 05'00" - 104°45'00"

X

1956 - present

8

Thanh Mai

18°37'59" - 105°22'00"

X

1960 - present

9

Vu Quang

18°22'43'' - 105°30'09''

X

1962 - present

Hydrometeorological data including: rain, evaporation, water level, flow are provided by the North Central Hydrometeorological Station. Daily rainfall data is synchronized from 1970 - 2019 at 28 stations. The study used 15 years of data (2005 - 2019) with a rainfall period of 6 hours. The total number of floods occurring in the downstream of the Ca River in the above 15 years was 23, the largest flood occurred in October 2010 with a flood peak of 4.96 m and the smallest flood occurred in September 2019 with a flood peak of 2.09 m at Cho Trang. In particular, flow data at Coc Na is only available from 1961-1976.


2.1.2. Topographic data

Baseline topographic data inherited from the Ministry of Natural Resources and Environment's Project " Research on detailed levels of natural disaster risks caused by flooding in urban areas and coastal plains in the North Central region " in 2019;

DEM map 1:10,000 of the entire Ca River basin inherited from the Project " Building a disaster-resilient society phase 2 - Nghe An province " implemented by JICA in 2014 [69].

2.1.3. Cross-sectional data

Cross-sections on the main rivers in Nghe An and Ha Tinh were received from the Hydrometeorological Survey Federation in 2001. The project " Developing a flood forecasting calculation program to serve the operation of the reservoir system in the Ca River basin" (2016) provided 70 additional cross-sections, including 56 cross-sections on the Ca River from the Dua TV station to Cua Hoi and 14 cross-sections on the La River from the Hoa Duyet TV station to the Cho Trang junction.

2.2. Analysis of factors causing flooding in the Ca River basin.

Factors causing natural disasters are often divided into 3 groups: endogenous, exogenous and anthropogenic. Specifically, in the Ca River basin and downstream of the Ca River, factors causing flooding are analyzed as follows:

2.2.1. Endogenous factors

2.2.1.1. Geographical location

The Ca River basin stretches from 18 0 15'50" to 20 0 10'30" North latitude, from 103 0 45'10" to 105 0 15'20" East longitude. The North borders the Chu River basin, the West borders the Mekong River basin, the South borders the Gianh River basin and the East borders the East Sea, on the territories of the two countries Vietnam and Laos, the total basin area is 27,200 km 2 , of which the area in Vietnam is 17,950 km 2 , accounting for 66.0% of the basin area; the area in Laos is 9,250 km 2 , accounting for 34.0% of the basin area. The main stream of the Ca River is 531 km long, of which 170 km flows in Laos and 361 km in our country ( Figure 2.2 ).


With its location near a large source of moisture, the East Sea, during the Northeast monsoon season, the basin has very favorable hydrological conditions, easily forming heavy rains, causing flooding in the downstream areas of the basin . In addition, the Ca River basin is also affected by the KKL mass in the North flowing down and the hot and humid air mass blowing up from the Bay of Bengal. With the single or mutual interaction combined with the influence of complex terrain, the Ca River basin has many different flood regimes: the upstream Ca River in Laos often has early floods from June to September; the Hieu River region often has floods from July to October; the La River region is later, from August to November.

2.2.1.2. Terrain

The Ca River basin has the following main terrain types:

- The high mountainous terrain is concentrated in the West, Northwest and Southwest of the basin. This terrain has an altitude of 800 ÷ 1,500 m, acting as a wall between the Mekong River basin and the Ca River basin. This terrain has steep slopes and narrow valleys, accounting for up to 60% of the basin area. This high mountainous terrain is favorable for the formation of heavy rain when there is moisture from the East Sea during the stormy season, causing floods in the Ca River basin ( Figure 2.2 ).

- The midland hills belong to the districts of Nghia Dan, Quy Hop, Tan Ky, Anh Son, Thanh Chuong (Nghe An), Vu Quang, Huong Son and Huong Khe (Ha Tinh) (Table 2.4 ), the total area of ​​this terrain is about 680,000 ha. This is a complex terrain, strongly divided with multi-directional slopes created by small rivers, with a general slope in the West - East, Northwest - Southeast, Southwest - Northeast direction and the lowest navel is the Ca River mouth. The average slope of the basin is large. The terrain of this area has a large slope both in the basin and in the riverbed with a large degree of division, creating conditions for the flow to quickly drain downstream, causing flooding. The terrain of the plains and coastal plains is small, narrow and close to the main stream. The plains from Do Luong down are protected by dikes on both banks of the river, except for the right bank of Thanh Chuong and Nam Dan which are protected by a dike. The plains in Ha Tinh from Vu Quang district to Duc Tho have no protective dikes.

42



Figure 2.2: River network in the Ca River basin


- Delta type, with a total area of ​​about 350,000 hectares, accounting for 10% of the Ca River basin area. The low-lying terrain in the delta with a cross-cutting traffic system and urbanization is a favorable condition for flooding when there is heavy rain in the fields .

2.2.1.3. Geology and soil

The Ca River basin is located in the Northern folded zone and the Indochinese Varixet folded zone, the boundary between the two folded zones is the Ma River suture zone. Studies in the monograph " Geological formations and geodynamics of Vietnam 1993 " edited by Nguyen Xuan Tung [75], classified the Ca River basin as located in the "Northern-Yangtze-KaTaZia area" between the Paleozoic North Truong Son continental crust belt. During the pre-Cambrian to early Paleozoic to late Paleozoic periods, the Ca River basin existed in the microcontinental oceanic regime, continental slope, and subcontinental regime. The rift and prerift regime existed during the late Paleozoic to late Merozoic periods. From the late Merozoic, small orogenic basins were formed along the Ca River fault, filled with coarse terrigenous sediments.

Soils in the basin have different origins. In mountainous areas, soils are developed on many types of lava. Most of the mountainous areas are below the altitude of 800 - 1,000 m, so they are strongly weathered. Ferralitic process is the main process. Ferralitic soil groups of hills and low mountains, distributed at altitudes below 800 - 1,000 m

1,000 m, occupies the largest area and is the place where human activities take place. The group of geologic soils, accounting for 83.5% of the entire basin, includes the following types: Red-yellow soil on shale, found on almost all types of terrain but concentrated in low mountainous areas, steep slopes, quite thick soil layer, soil layer thickness is mostly over 50 cm. This is a type of hilly soil with good water retention and color retention properties; Light yellow soil develops on sandstone and conglomerate. Due to its lighter mechanical composition than shale, this type of soil is often strongly eroded, the soil layer is relatively thin and many places are bare of gravel and rock. Only a few places have high hilly terrain, carpet


The relatively new vegetation cover has a soil layer thickness of 50-70 cm. This type of soil has poor water retention and adhesion; Red-yellow soil develops on acidic rocks. Most of this type of soil has light mechanical composition, poor in nutrients, and is strongly eroded and washed away, so its water retention capacity is poor; Red-brown soil on limestone, in contrast to other types of soil, this type of soil in low-lying areas often has a thicker soil layer, in high-lying areas it is often weathered and washed away strongly, so the soil layer is thinner. Therefore, this type of soil has better water retention capacity; Red-brown basalt soil, mainly distributed in Phu Quy area. This type of soil has a layer thickness of over 1 m, the terrain is quite flat, highly fertile, loose, well-drained but retains water poorly; Red-yellow Feralit soil on the mountain, humus soil on high mountains, this type of soil accounts for 29.0% of the soil area. Although it has high fertility, because it is mainly concentrated in high mountains, steep terrain and is strongly fragmented, its water retention capacity is also limited [76].

Figure 2.3: Soil map of Ca River basin (Vietnam part)

In the plains, the soil is formed from river alluvium consisting of groups of

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