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SECAO 2 ANTECEDENTES GEOGRAFICOS, PANTANAL E HIDROVIA Esta secao estabelece os antecedentes geograficos para este estudo. Esta dividida em quatro subsecoes: 1.A Bacia Hidrografica do Paraná-Paraguai 2.As Bacias Hidrograficas do Paraguai e Alto Paraguai 3.O Pantanal Matogrossense 4.O Projeto da Hidsrovia Paraná-Paraguai (Hidrovia). Este estudo focaliza o impacto do projeto proposto da hidrovia Paraná-Paraguai no Pantanal Matogrossense, o qual se situa na bacia do Rio Paraguai, um tributario impor tante do sistema hidrografico Paraná-Paraguai. As fontes de referencia para as informa coes contidas nesta Secao estao listadas no Apendice 1. As figuras e tabelas para todas as Secoes estao incluidas nos Apendices 2 e 3, respectivamente. 2.1 A Bacia Hidrografica do Paraná-Paraguai A bacia hidrografica do Paraná-Paraguai e a mais importante do sistema do Prata em termos de descarga (75 %) e area de drenagem (84 %) (Bonetto, 1975). O sistema do Rio da Prata e o segundo maior de America do Sul, depois do Amazonas. A bacia do Paraná-Paraguai drena uma regiao extensa, compreendendo 2605 000 km2 no Brazil, Argentina, Paraguai e Bolivia. Como seu nome indica, e composta de dois rios principais: o Paraná e o Paraguai. O Paraná e o maior dos dois, drenando 1510 000 km2 (58 %) da bacia. O rio Paraguai, drenado os 1095 000 km2 restantes, e o tributario mais importante do rio Paraná. A distribuicao geografica da bacia do rio Paraná re a seguinte: 59 % no Brasil, 37.4 % na Argentina e 3.6 % no Paraguai. A distribuicao geografica da bacia do rio Paraguai e: 33.3 % no Brasil, 33.3 % no Paraguai, 16.7 % na Argentina e 16.7 % na Bolivia (Anderson et al, 1993). A bacia hidrografica combinada dos rios ParanáParaguai drena uma parte significativa desses quatro paises Sul Americanos (Figura 1). O rio Parana esta dividido em tres secoes distintas (Bonetto, 1975): 1.O Alto Paraná, das cabeceiras do rio Paraná nas vizinhancas de Brasilia, ate a con fluencia com o rio Paraguai. 2.O Medio Paraná, da confluencia com o rio Paraguai ate o porto de Diamante, perto de Santa Fé, Argentina, uma distancia de cerca de 700 km. 3.O Baixo Paraná, de Diamante ate o estuario do rio da Prata, uma distancia de aproximadamente 400 km. 2.2 As Bacias Hidrograficas do Paraguai e Alto Paraguai As cabeceiras da bacia do rio Paraguai estao localizadas na serra de Tapirapuã, nas proximidades da Vila de Parecis, no estado de Mato Grosso (EDIBAP, 1979). Depois de escoar geralmente na direcao Sul por uma distancia de cerca de 2800 km, o rio Paraguai alcanca o Paraná em Confluencia, ao norte das cidades Argentinas de Corrientes e Resistencia (Figura 1). O rio Paraguai esta dividido em tres secoes (Anderson et al, 1993): 1.O Alto Paraguai, escoando a traves do Brasil, Bolivia e Paraguai, das suas cabecei ras ate a confluencia com o rio Apa, uma distancia de 1873 km. 2.O Medio Paraguai, escoando a traves de Paraguai e Argentina, da confluencia com o rio Apa ate a confluencia com o rio Tebicuary, uma distancia de 797 km. 3.O Baixo Paraguai, atravessando o Paraguai e Argentina, da confluencia com o rio Tebicuary ate a confluencia com o rio Paraná, uma distancia de 130 km. Os rios Pilcomayo e Bermejo, tributarios do Medio e Baixo Paraguai, respectiva mente, descem dos Andes para o Oeste (Figura 1). Similarmente, os tributarios orientais do Medio e Baixo Paraguai escoam sobre relevo montanhoso. O restante da bacia do rio Paraguai compreende uma imensa planicie interior, com relevo extremadamente plano. Essa disposicao geomorfologica peculiar causou a existencia do Pantanal Ma togrossense, um extenso grupo de alagadicos localizado integralmente na bacia do Alto Paraguai (Tricart, 1982). O trecho Alto Paraguai e a secao mais a montante do rio Paraguai, das suas cabecei ras ate a confluencia com o rio Apa. Esse ultimo define a fronteira entre o Brasil (ao Norte) e Paraguai (ao Sul). A bacia do The Upper Paraguay river basin contains the Pan tanal of Mato Grosso and its headwaters, wholly within Brazilian territory, and portions of Eastern Bolivia and Northwestern Paraguay. While the precise western limits of the basin are uncertain (the Bañados de Izogog, in Eastern Bolivia), the northern and east ern limits are delimited by mountain ranges, all within Brazil. To the East, the basin is limited by the Maracaju, Caiapó, and Saudade ranges; to the North by the Parecis range, and partly by the Azul range. The basin lies between 14o and 23o S, and 53o and 60o W (Fig. 2). The Upper Paraguay river basin comprises 496 000 km2, in two distinct regions (DNOS, 1974): 1.The area to the left (west) of the Paraguay and Jauru rivers, wholly within Brazilian territory, encompassing 336 000 km2; half of this area is above the altitude of 200 m. 2.The area to the right (east) of the Paraguay and Jauru rivers, encompassing 160 000 km2, of which 145 000 km2 are in Bolivian and Paraguayan territory, and the re maining 15 000 km2 are in Brazil; 19 percent of this area (31 000 km2) is above the altitude of 200 m. The principal tributaries of the Upper Paraguay river are (Fig. 2): 1.Sepotuba, 2.Cabaçal, 3.Jauru, 4.Cuiabá, and its tributaries São Lourenço and Piquiri-Itiquira, 5.Taquari, and 6.Miranda, and its tributary the Aquidauana. Other tributaries, primarily intermittent, include the Negro, Aquidabã, Branco, Tereré, and Amonguijá. All these are left-bank tributaries, located wholly within Brazil. For reference purposes, Table 1 shows selected hydrographic characteristics of the Upper Paraguay river. Table 2 shows selected hydrologic data at gaging stations along the Upper Paraguay river (Fig. 3). Table 3 shows valley slopes along the Upper Para guay river and its major tributaries. Table 1 shows that the Upper Paraguay river is quite sinuous, particularly upstream of Corumbá, where the sinuosity, i.e., the ratio of river length to valley length, can be quite high. For instance, the reach from 40 km downstream of Porto Conceição to Refúgio das Três Bocas, where the sinuosity is: 161 km/55 km = 2.92. The influence of sinu osity on proposed navigational improvements is analyzed in Section 4.1.1. Table 2 shows that the difference between maximum and minimum observed water levels along the Upper Paraguay river is smallest at Descalvados (2.61 m), remaining small (less than 3.5 m) for about 200 km downstream (at Porto Conceição it is 3.28 m; at Bela Vista do Norte it is 3.27 m). This indicates the presence of substantial channel overflows in the Upper Paraguay river between Descalvados and Bela Vista do Norte. Table 3 shows that valley slopes in the Upper Paraguay river basin decrease gradually, from 15-50 cm/km close to the mountains to the north, east, and south, to 7-15 cm/km along the major tributaries, and to 0.7-6.5 cm/km along the Upper Paraguay river. This reveals that the Upper Paraguay river constitutes a regional base level for the flow of its eastern tributaries. 2.3 The Pantanal of Mato Grosso The Pantanal of Mato Grosso is a seasonally inundated depression wholly contained within the Upper Paraguay river basin, encompassing approximately 136 700 km2 (Pro jeto RADAMBRASIL, 1982a&b). The Pantanal is geomorphologically and hydrologi cally positioned to attenuate and reduce the runoff from the basin. Tricart (1982) has stated that the mountains to the south of the Pantanal "strangle" the valley of the Upper Paraguay river close to the location where it exits Brazilian territory. Significantly, this geomorphic feature is referred to locally as Fecho dos Morros, literally, "closing of the hills." (Fig. 3). The Pantanal is a huge natural reservoir receiving distributed inflows from the Upper Paraguay river and its tributaries, and concentrating runoff at the basin outlet, the Apa river confluence, about 100 km downstream of Fecho dos Morros. Large portions of the Pantanal are flooded only during the annual crest of the Upper Paraguay river and its tributaries, and much nonflooded terra firma is interspersed throughout the region. The mixture of permanent swamp, seasonal swamp, and non flooded land, as well as the contiguity of the Pantanal to major South American biomes (the humid Amazon rainforest to the north and northwest, the subhumid savannas of Central Brazil to the east, the humid Atlantic forest to the southeast, and the semiarid scrub forest of neighboring Bolivia and Paraguay to the west and southwest) have condi tioned the richness and variety of its vegetation and climate (Prance and Schaller, 1982). In turn, the Pantanal ecosystems support a rich and diverse fauna, including numerous species of mammals, reptiles, fish, birds, butterflies, and other invertebrates (Brown, 1986). The name Pantanal of Mato Grosso tends to hide the fact that the depression of the Upper Paraguay basin consists of not one but several seasonally flooded regions, quite distinct from each other; thus, the Portuguese name Planícies e pantanais Matogros senses, which stands for "Plains and swamps of Mato Grosso." The following pantanais were identified by Projeto RADAMBRASIL (1982a&b) (Fig. 4): Corixo Grande-Jauru-Paraguay, (2) Cuiabá-Bento Gomes-Paraguaizinho, (3) ItiquiraSão Lourenço-Cuiabá, (4) Paiaguás, (5) Taquari, (6) Jacadigo-Nabileque, (7) MirandaAquidauana, (8) Negro, (9) Tarumã-Jibóia, (10) Aquibadã, (11) BrancoAmonguijá, and (12) Apa. Alternatively, Adámoli (1981) has classified the Pantanal of Mato Grosso into ten pan tanais: (1) Cáceres, (2) Poconé, (3) Barão de Melgaço, (4) Paiaguás, (5) Nhecolândia, (6) Aquidauana, (7) Paraguay, (8) Miranda, (9) Nabileque, and (10) Abobral. The peculiar characteristics of the pantanais have led to the use of regional terminol ogy to describe its most salient geomorphic features, namely baías, baixadas, barreiros, salinas, córregos, capões, cordilheiras, vazantes, and corixos. A brief description of each follows. ·The baías are lowlying areas of circular, semicircular, or irregular shape, which have standing water, sometimes saline; their linear dimensions vary from tens to hundreds of meters. ·The baixadas are portions of the baías subject to seasonal inundation (Silva, 1990). ·The barreiros are baías that have seasonal or periodic water (Valverde, 1972). ·The salinas are lakes with saline water; they are covered during the dry season with salt crusts, and are for the most part unconnected from the seasonally flooded baías (Silva and Pinto-Silva, 1989). ·The córregos are small watercourses (Carvalho, 1986). ·The capões are vegetated earthmounds, of various sizes, and approximately circular or elliptical in shape (Ponce and Cunha, 1993). ·The cordilheiras are slight terrain elevations located between the baías, with mean elevations about 2-3 m above the water level in the baías. While they are normally dry, they are subject to inundation during exceptional floods. They serve as high areas for the location of cattle ranches, and as refuge for livestock during extraordi nary and exceptional floods. ·The vazantes are large depressions situated between the cordilheiras, lacking a clearly defined channel (Carvalho, 1986). During the flood season, these depressions drain intermittent streams, extending for several kilometers. However, many vazantes are perennial, revealing the presence of substantial amounts of subsurface flow. ·The corixos, unlike the vazantes, are small permanent watercourses connecting adja cent baías with narrower and much deeper channels. When the corixo is long and has a well defined cross section, it is referred to as corixão (Carvalho, 1986). The characteristics of the several pantanais that constitute the Pantanal of Mato Grosso are described by Projeto RADAMBRASIL (1982a&b) and Silva (1986). The soils and inundation patterns (flooding levels) of the Pantanal are described by Projeto RA DAMBRASIL (1982a&b) and Amaral Filho (1986). 2.4 The Paraná-Paraguay Waterway (Hidrovia) Project The Paraná-Paraguay river basin system is an extensive region in South America, which lies within the countries of Argentina, Bolivia, Brazil, and Paraguay. The neigh boring Uruguay river drains portions of Argentina, Brazil, and Uruguay. The confluence of these two rivers is near the city of Nueva Palmira, Uruguay (Fig. 1). The ParanáParaguay and Uruguay rivers are the major tributaries of the La Plata basin system. The Paraná-Paraguay basin is home to a population of almost 20 million people. For centuries, this river system has been used as a waterway for transportation. In February 1995, the IDB and the UNDP commissioned an 18-month series of engineering and en vironmental impact studies to evaluate potential navigational improvements to the exist ing waterway. This study includes the possibility of extensive engineering works to render 3442 km of the river navigable for ocean-going vessels, from Nueva Palmira to Cáceres, Brazil. Since the port of Cáceres is located upstream of the Pantanal of Mato Grosso, the short- and long-term impacts of the proposed navigational im provements on the Pantanal should be clearly established prior to project implementation. The project is commonly referred to as the Hidrovia project, since "Hidrovia" means waterway in both Spanish and Portuguese. The stated purposes of the Hidrovia project are to enhance current river transport via improvements to existing port, channel, and navigation facilities and to construct a year-round navigable waterway along the 3442 km. These efforts are being planned in two stages: Phase 1 (Module A): Short-term intervention This phase entails the improvement in navigational aids and the required river engi neering, including dredging and related works, along 80 percent of the proposed pro ject's length. The affected region extends from the downstream port of Nueva Palmira, upstream to the port of Corumbá/Ladario, in Brazil, and neighboring Puerto Quijarro, in Bolivia. Phase 2 (Module B): Medium- and long-term intervention This phase entails the improvement in navigational aids and the required river engi neering, including dredging, channel modification, and other major river interventions, along the entire length of the proposed project (3442 km), from Nueva Palmira to Cáceres. The executive agency for the Hidrovia project is the Comité Intergubernamental de la Hidrovia (CIH) (Intergovernmental Committee of the Waterway), established in 1989 by the Ministers of Public Works and Transport of Argentina, Bolivia, Brazil, Paraguay, and Uruguay. The headquarters of the CIH is in Buenos Aires, Argentina. To date, the only comprehensive document with enough detail on the Hidrovia pro ject is the Internave report, commissioned by the extinct Empresa de Portos do Brasil (PORTOBRAS), and completed in 1990 by the Brazilian company of the same name (INTERNAVE, 1990). This report is basically an economic feasibility study of the Hidro via project. As such, it uses projections of economic benefits to justify the costs involved in project implementation. The Internave report has been criticized for its overly optimistic projections of benefits (CEBRAC/ICV/WWF, 1994). The IDB has formally rejected the Internave study and will use the Phase 2 feasibility study, currently under execution, to recalculate cost and benefits (Lammers et al, 1994). However, the physical descriptions contained in the Internave report, which include channel straightening, dredging, blasting of rock out crops and other structural interventions in the river, some of them irreversible, have re mained the cause for significant concern among diverse segments of the local, national and international communities. These include environmental organizations, nongovern mental organizations (NGO's), professional associations, and universities and scientific re search institutions in Brazil, the American continent, and the rest of the world. Channel straightening by realignment and cutoffs, dredging, and blasting of rocky sills are being considered to improve navigational conditions along the waterway. In particu lar, the Terms of Reference of the Phase 2 (Module B-1) engineering study, under Section 1--Purpose, states the following task (No. 4), among seven others (IDB, 1995, p. 2): The extent of these interventions and their possible impact on the hydrologic regime of the Pantanal of Mato Grosso will be better known by the second half of 1996, once the ongoing studies are completed. The IDB has asserted that it may not fund the Hidrovia project through the Pantanal if serious environmental impacts are anticipated (Lammers et al, 1994). Thus, the present study is a contribution to the proper assessment and evaluation of these impacts. The Internave report lists the various geographic locations along the Hidrovia project, starting from the port of Buenos Aires (Km 0), progressing upstream to the port of Cáceres (Km 3 442). For reference purposes, an abstracted list of locations relevant to this study is shown in Table 4. Minor discrepancies between river distances in Tables 1 and 4 reflect the different sources for these tables: DNOS (1974) and INTERNAVE (1990). _ _ _