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Yangtze River (Changjiang River, 长江)

About Yangtze River: The turbid water impresses with its yellow-brown color

the visits before and during the construction of the three gorges dam

Yangtze-TeubnerYangtze River, at Nanjing, 2004:
The lower stretch is an important waterway. Large  vessels are able to navigate this stretch.
Yangtze-TeubnerYangtze River, middle stretch 2004:
Traditional Chinese river sailing boats, called 'junks' are seen on the stony-rocky river shore. The boats are of different sizes having only one, two or three sails, respectively.

Yangtze-TeubnerYangtze River, at Nanjing, 2004:
This roll-on/roll-off port near a village is built for a small double ended vehicle ferry (see S). 
Yangtze-TeubnerYangtze River, middle stretch 1997:
Traditional Chinese boats with lift nets are going fishing on the river near Chongqing. Such scenery with fisher boats on Yangtze River was only seen during the visit in 1997, not in 2004. A detailed description of the operation of lift nets on fisher boats is given on this website for a tributary of Yantze River at Yichang, the Huangbai, visited in 2004 (Yichang S).

For the largest River in Asia, Yangtze River (also called Changjiang River or Yangzi River), the ecosystem properties are as manifold as the long river channel diversity is (see also ‘the many faces’ of the mountain stream Shennong Xi S, which is a tributary of the Yangtze River, described on this lakeriver-website). A few photos shown here are from the broad channel of Yangzte River downstream the city Nanjing. The majority of photos, however, illustrate the middle stretch from Yichang to Chongqing, passing the Three Gorges. Photos taken here are labeled according to sections Yichang-Badong and Badong-Chongqin stretch, respectively. The photo 70 in the top gallery shows a tourist map with main cities and viewpoints along the river that was displayed on a river cruise ship in 2004. The photos were mainly taken in 2004, when the Three Gorges Dam has been under construction with the aim to bring up the water level to 175 m (see the water level mark on the photo in the paragraphs below). At that early stage of dam construction in 2004, the water level had been already reached 136 m (see more detail below). In addition some photos that were taken in 1997 were selected to show the riverbed many years before the dam construction has been started. The damming up of Yangtze River increased not only the water level of the main river channel, but also of its tributaries as e.g. of the Shannon Xi mentioned before. Some scenes shown by photos on this website are today beneath the reservoir’s water level. In case of the Shibaozhai, which was still above the water when the dam construction was already ongoing in 2004, a wall protects now the small island of the temple complex from water. Another photo taken in 1997 shows traditional wooden fisher boats with lift nets seen on the main channel from the river. For another tributary of Yangtze River, the Huangbai River at Yichang S, the fishing with the lift net is illustrated in great detail from the visit in 2004. Traditional fisherboats with lift nets were also common on lakes, as shown for lake Dianchi S on this website in 2000/2001.

Yangtze-TeubnerYangtze River, Qutang Gorge, 1997:
The four cliff inscriptions seen in this photo were engraved on the 'Chalk Wall' in different eras. At the time before the water level rise started due to the dam project, they were seen close down to the water's edge of Yangtze. The green painted inscriptions on the left side, for example, were written with traditional characters of gently curved lines. Someone has been taken care to maintain these historical inscriptions such as those, for instance, with the large-size characters in red color are obviously looking freshly painted. On the screen-sized photo that you get by mouse double-click, all four inscriptions are seen on detailed inserts and can be easily read.
Yangtze-TeubnerYangtze River, BaiDi Cheng - White Temple, 2004:
The main picture shows a water colour painting exhibited on the White Emperor City. A young woman, who is carrying a child in a sling, is preparing fish for drying on air (stockfish, see also Taihu S).
Left insert: Wall modeling of the main entrance gate of the White Temple: A water buffalo is used for ploughing the field. Such buffalos were common livestocks in the Yangtze River basin (see also water buffalos on Yangtze tributary Shannon Xi S and lake Poyang S).
Right insert: Fish sculpture as modern art craft by local people from Yichang.

Yangtze-TeubnerYangtze River, Qutang Gorge, 1997:
Scenic view from the boat at the White Temple (White Emperor City) onto the gorge.

Yangtze-TeubnerYangtze River, Shibaozhai temple, 2004:
Scenic view from the temple onto the river at dusk. At that early stage of the Three Gorge Dam construction, the temple complex yet remains above the water level.

Yangtze River cruises have been popular over many years. The four photos below depict the cruise ships passing the ship lock at Gezhouba Dam at Yichang and the further upstream section. The following six photos relate to the cruise passage at the Three Gorges Dam.

Yangtze-TeubnerPopular river cruises on Yangtze, 2004:
The ship locks at the Gezhouba Dam were built for large vessels. The ships are taken upward and downward to master the different water level rise of about 21 to 25 (?) m.
Yangtze-TeubnerPopular river cruises on Yangtze, 2004:
The ship is raised in the ship lock at Yichang. People enjoy the time on board of the cruise ship.

Yangtze-TeubnerPopular river cruises on Yangtze, 2004:
These large vessel are able to navigate through the midstretch of the river. The river passes here rocky banks that look most impressive.
Yangtze-TeubnerPopular river cruises on Yangtze, 2004:
Hot water is all time freely available on board. In the past when people suffered from having not enough to eat and drink, plain 'hot water'  was called 'white tea'.

The following four photos give an impression about the huge construction of the Three Gorges Dam. The ships shown here are lifted up through the passage of water level rise by passing five locking steps. Before the rise in water levels resulting from the construction of the new reservoir, housing areas and factories had to be removed from the river shore (see photos below but also photos 32 and 60-64 in the top gallery). As a consequence, during this early stage of the dam project in 2004, deserted areas could be seen along the middle stretch of the Yangtze River. The slope installations of water level gauge boards and the signs for the 175 m were placed at many river sections and indicated the final water level reached by the Three Gorge Dam construction. The photos taken in 2004 are thus taken before the water level further rises another 39 m.

Yangtze-TeubnerYangtze River, 2004:
View on the model of the Three Gorges Dam with five locking steps.
Yangtze-TeubnerYangtze River, 2004:
The pair of five ship locks is seen. Three cruise vessel enter the locks to pass the water level rise due to the Three Gorges Dam.

Yangtze-TeubnerYangtze top lock of the five lock steps of 2004:
The vessels pass the top gate going further upstream.
Yangtze-TeubnerYangtze River, Three Gorges Dam, 2004:
View back on the pair of locking steps on the left, and the Three Gorges Dam on the right side.

Yangtze-TeubnerSloping installation of a water level gauge board on the mid strech of Yangtze River, 2004:
With the construction of the Three Gorges Dam, the water level rises finally to 175m. At that early stage of the dam project, in 2004, the water level of 136m has already been reached.
Yangtze-TeubnerYangtze River, 2004:
Deserted housing area in advance of the water level rise due to the construction of the Three Gorge Dam.

the low water transparency at the main channel of yangtze river inhibits the growth of algae and other phytoplankton species

The yellow-brownish color of the water of the Yangtze River and lakes in the Yangtze River basin (e.g. such as Poyang Lake S, turbidity at low and high water level seasons of this large lake see Liu et al. (2016) R is perhaps the most impressive aspect of their specific ecology. The extreme water turbidity is mainly due to high concentrations of suspended solids (silt) washed in by soil erosion from the surrounding landscape. The low water transparency becomes obvious simply by dipping in a plankton net, which optically disappears few millimetres beneath the water surface. To study algae in a plankton sample that contains that large amount of suspended solids is challenging as photosynthetic microorganisms are rare in the sample and overcrowded by plenty of inorganic particles from soil and sediment. The extraction method of analyzing photosynthesis pigments might be here the more straightforward measure of estimating their biomass than counting these microorganisms under a light microscope. A common extraction method is to analyse quantitatively chlorophyll-a, as all planktonic primary producers, i.e. algae and cyanobacteria, build this photosynthetic pigment (Greisberger & Teubner 2007 R). The concentration of chlorophyll-a is thus used as a rough estimator for total biomass of the photosynthetic microorganisms in a plankton sample.

Yangtze-TeubnerYangtze River, downstream at the city Nanjing, 2004:
Dipping in the plankton net illustrates how low the transparency of the river water is.
Yangtze-TeubnerYangtze River, mid-stream, 2004:
Karst landscape is bordering the river channel. Here the vegetation cover does not prevent soil erosion on the steep slopes. Coarse gravel is seen on the river bank.

Yangtze-TeubnerYangtze River, mid-stream, 1997:
The wide shallow river shore is a result of both soil erosion and soil sedimentation. The bordering landscape is used for growing crops.

Yangtze-TeubnerYangtze River, mid-stream, 1997:
The karst landscape in 1997 looks looks similar to the photo above, taken 7 years later when the dam construction in progress. The original river shore shown here, however, typically appeared shallower and wider and contained more fine than coarse material as depicted here.

A huge algal biomass in a flushed turbid river, in principle, cannot be expected. The higher the flow velocity of a river and the lower the water transparency is (i.e. a lowered availability of photosynthetically active radiation) the less photosynthetic microorganisms will grow in the river, regardless of the nutrient concentration in the river. In other words, whereas planktonic algae are a good predictor for nutrient enrichment in lakes, this is not the case in running waters. In rivers of higher flow velocity, the number of algal cells is lower than in lakes with the same nutrient level as cell division is mechanically inhibited in the river, and further cells are washed out. In contrast to the situation in rivers, an increase of nutrient concentrations in lakes is usually promptly responded to by algal growth as is commonly seen by the evolution of green algal blooms with nutrient enrichment in lakes (eutrophication of lakes). Observing growth of photosynthetic microorganisms in natural habitats implies that cells undergo cell divisions. Under unlimited growth conditions during exponential growth periods, e.g. in spring, about one cell division every day can be expected in a lake (exponential growth phase in the spring).

Yangtze-TeubnerYangtze River, 2004:
Terracing to prevent soil erosion. 
Yangtze-TeubnerRiver bank of Yangtze, 2004:
Crops on terraces: the harvest of sesame. Insert: matured fruits with seeds of sesame plant.

Despite of the growth-inhibiting effects of high flow-velocity on algae, some algae can be even found in the main channel river plankton. These algae often originate from habitats of longer retention time connected to the river, such as from small bay habitats at the river shoreline of a main stretch, from river side arms or even lakes. In the situation where nutrient-rich river water enters a broadened stretch or dam reservoir, the water residence time increases. As a consequence the huge amount of suspended solids deposits immediately and in turn water transparency increases. Sufficient light availability for photosynthesis in addition to enhanced nutrient concentration accumulated by the river stimulates algal growth and may promptly even turn the water colour from sediment-brownish to algal-green in a reservoir or lake (see details about Meiliang Bay of the north of lake Taihu and related publications by Chen et al. 1993 R and 1993 R discussed on the website for the Shennong Xi S, see also the page about lake Taihu S).

Yangtze-TeubnerYangtze River, 2004:
Chamber of a ship lock. The dark-green color of the wall is mainly due to the both photosynthetic pigments phycocyanin and chlorophyll-a that are synthesized by micro-organisms. The 'Blue-Greens', i.e. cyanobacteria, built here the biofilm on the wall in addition to other aquatic micro-organisms as algae and bacteria.

Yangtze-TeubnerYangtze River, 2004:
The blue-green color of the wall of the ship lock chamber is due to attached living cyanobacteria as described for the left photo. The filamentous colonies of these photosynthetic micro-organisms can be macroscopically seen (see screen-sized photo). Other photosynthetic micro-organisms, as e.g. unicellular diatoms, also inhabit the biofilm, but are too small and hence can be observed only under a light microscope.

While photosynthesis and thus the growth of floating algae in the turbid water are inhibited, the photosynthetic micro-organisms attached to the wall of chambers of ship locks seen on the photos above can obviously grow well. The wall looks dark-green due to the biofilm built by the ‘blue-greens’, the cyanobacteria. In addition to chlorophyll-a, many cyanobacteria also produce blue-green photosynthetic pigments, the ‘turquoise blue-green’ phycocyanin. The growth of the cyanobacteria seen on the wall seems to correlate well with the fluctuating water level. The time-intervals of recurrent emptying of the chamber are long enough to satisfy daily photosynthesis with sufficient light. The underwater darkness by flooding the ship lock chamber might interrupt photosynthesis but provides access to the nutrients that are dissolved in the water. When the ship lock chamber is emptied again, sufficient light for photosynthesis becomes available and a thin water layer on the wet wall serves as ‘nutrient solution/growing medium’. The uptake of some nutrients as phosphorus depends on energy provided by photosynthesis and thus can only succeed during ‘day-time’ and ceases immediately at night or darkness. Cyanobacteria and other primary producers, however, are able to utilize even small concentrations of phosphate close to the chemical detection limit within few minutes. Cyanobacteria can benefit from different environmental conditions by various survival strategies, as e.g. by the adjustment to light availability, and by the switch between an autotrophic and heterotrophic life-style.

Cyanobacteria are known to grow well even on rocks when water is just available from time to time by rainfall. The cyanobacteria can build different types of mucilage as for example described for planktonic Microcystis colonies on this website for lake Taihu S. In particular, thick mucilage layers are usually built by cyanobacteria, not living planktonically, but attached on stones in the splash of a stream or on steep slopes of mountain rocks. The mucilage that envelops the cyanobacterial cells protects then against drying out too rapidly, damage by UV and being washed out. A cyanobacterium, which is found globally on soil and can even survive longer dry periods, is Nostoc commune and is further illustrated on this website.

Cyanobacteria are commonly associated with bacteria and other photosynthetic microorganisms, floating or drifting in the water (phytoplankton) or living attached to the substrate as stones on the shore (phytobenthos). The association of various species living together can be very close. The enveloping mucilage produced by the planktic Microcystis and that thus belongs to the Microcystis aeruginosa colony, can serve further as a habitat for other species such as diatoms (Navicula) and other cyanobacteria (Pseudanabaena mucicola, see micrographs on page 48/49, Plate I, fig.2 in Teubner, 1996 R). In addition to the benthic cyanobacteria, mainly benthic diatoms that also produce sticky mucilage are commonly found in biofilms. The unicellular benthic micro-organisms can usually move in their micro-habitat. They are able to glide to places, there are not many shadows but also not too much light. In this way, the organisms can avoid the both extremes, namely growth limitation by low light internsity and cell damage by excessive light, respectively. Watching a live sample under the light microscope, the speedy movement of pennate diatoms or filamentous cyanobacteria gliding on the glass slide can be seen. It is known for pennate diatoms living attached on stems of reed in the littoral, that they change their position by migrating around the stem following the angle of incidence of the sun.

cited References on this site about Yangtze River

Liu X, Teubner K, Chen Y (2016) Water quality characteristics of Poyang Lake, China, in response to changes in the water level. Hydrology Research, in press DOI:10.2166/nh.2016.209 OpenAccess 

Greisberger S, Teubner K (2007) Does pigment composition reflect phytoplankton community structure in differing temperature and light conditions in a deep alpine lake? An approach using HPLC and delayed fluorescence (DF) techniques. Journal of Phycology 43:1108-1119 doi:10.1111/j.1529-8817.2007.00404.x Look-Inside FurtherLink 

Chen Y, Qin B, Teubner K, Dokulil MT (2003) Long-term dynamics of phytoplankton assemblages: Microcystis-domination in Lake Taihu, a large shallow lake in China. Journal of Plankton Research 25 (1):445-453 Abstract Abstract in Chinese OpenAccess

Chen Y, Fan C, Teubner K, Dokulil MT (2003) Changes of nutrients and phytoplankton chlorophyll-a in a large shallow lake, Taihu, China: an 8-year investigation. Hydrobiologia, 506:273-279 Abstract OpenAccess

Teubner K (1996) Struktur und Dynamik des Phytoplanktons in Beziehung zur Hydrochemie und Hydrophysik der Gewässer: Eine multivariate statistische Analyse an ausgewählten Gewässern der Region Berlin-Brandenburg. Ph.D thesis, Dept. Ecophysiology, Humboldt University Berlin: 232 pp Look-Inside FurtherLink