Final Report Irrigation Management and Crop
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Fit.* IRRIGATION and MULTI-PURPOSE DEVELOPMENT
fit.* The Historic Jaya Ganga — built by King Dbatustna in tbi <>tb century AD to carry the waters of the Kala Wewa to the ancient city tanks of Anuradbapura, 57 miles away, while feeding a number of village tanks in its course. This channel is also famous for the gentle gradient of 6 ins. per mile for the first I7 miles and an average of 1 //. per mile throughout its length. Both tbeKalawewa andtbefiya Garga were restored in 1885 — 18 8 8 by the British, but not to their fullest capacities. New under the Mabaweli Diversion project, the Kill Wewa his been augmented and the Jaya Gingi improved to carry 1000 cusecs of water. The history of our country dates back to the 6th century B.C. When the legendary Vijaya landed in L->nka, he is believed to have found an island occupied by certain tribes who had already developed a rudimentary sys tem of irrigation. Tradition has it that Kuveni was spinning cotton on the bund of a small lake which was presumably part of this ancient system. The development of an ancient civilization which was entirely depen dent on an irrigation system that grew in size and complexity through the years is described in our written history. Many examples are available which demonstrate this systematic development of water and land re sources throughout the so-called dry zone of our country over very long periods of time. The development of a water supply and irrigation system around the city of Anuradhapuia may be taken as an example. -
An Assessment of the Water Quality in Major Streams of the Madu Ganga Catchment and Pollution Loads Draining Into the Madu Ganga from Its Own Catchment
An assessment of the water quality in major streams of the Madu Ganga catchment and pollution loads draining into the Madu Ganga from its own catchment A.A.D. Amarathunga* and N. Sureshkumar National Aquatic Resources Research and Development Agency (NARA), Crow Island, Colombo 15, Sri Lanka. Abstract The Madu Ganga Lagoon is located in the Southern Coast, Northwest of the city of Galle within the Galle District. The aim of this study was to evaluate the pollution status of the lagoon and the contribution of the land base pollutants from the catchment of the Madu Ganga. Selected water quality parameters were measured at monthly intervals at twelve sampling locations in the catchment. Certain parameters such as salinity (2.2 + 1.7 ppt), oil & grease (8.5 + 6.5 mg/L), total suspended solids (16.1 ± 12.3 mg/L), and turbidity (20.1 ± 12.5 NTU) are found to be elevated levels when compared with water quality standards. The study revealed that the Lenagala Ela brought a high nutrient load (426.7 kg/day) into Madu Ganga and Arawavilla Ela, Magala Ela and Bogaha Ela also contributed significantly. The highest nutrient loads were found with the onset of the Northeast Monsoon during November to January. The increase in nutrient loads is attributed to the fertilizers added to the soil with the commencement of the major paddy cultivation season. Keywords: Physico-chemical parameters, Madu Ganga, Water pollution, Nutrient load, Suspended sediment ^Corresponding author - Email: deeptha(s>nara.ac.lk, [email protected] Journal of the National Aquatic Resources Research and Development Agency, Vol. -
The Government of the Democratic
THE GOVERNMENT OF THE DEMOCRATIC SOCIALIST REPUBLIC OF SRI LANKA FINANCIAL STATEMENTS OF THE GOVERNMENT FOR THE YEAR ENDED 31ST DECEMBER 2019 DEPARTMENT OF STATE ACCOUNTS GENERAL TREASURY COLOMBO-01 TABLE OF CONTENTS Page No. 1. Note to Readers 1 2. Statement of Responsibility 2 3. Statement of Financial Performance for the Year ended 31st December 2019 3 4. Statement of Financial Position as at 31st December 2019 4 5. Statement of Cash Flow for the Year ended 31st December 2019 5 6. Statement of Changes in Net Assets / Equity for the Year ended 31st December 2019 6 7. Current Year Actual vs Budget 7 8. Significant Accounting Policies 8-12 9. Time of Recording and Measurement for Presenting the Financial Statements of Republic 13-14 Notes 10. Note 1-10 - Notes to the Financial Statements 15-19 11. Note 11 - Foreign Borrowings 20-26 12. Note 12 - Foreign Grants 27-28 13. Note 13 - Domestic Non-Bank Borrowings 29 14. Note 14 - Domestic Debt Repayment 29 15. Note 15 - Recoveries from On-Lending 29 16. Note 16 - Statement of Non-Financial Assets 30-37 17. Note 17 - Advances to Public Officers 38 18. Note 18 - Advances to Government Departments 38 19. Note 19 - Membership Fees Paid 38 20. Note 20 - On-Lending 39-40 21. Note 21 (Note 21.1-21.5) - Capital Contribution/Shareholding in the Commercial Public Corporations/State Owned Companies/Plantation Companies/ Development Bank (8568/8548) 41-46 22. Note 22 - Rent and Work Advance Account 47-51 23. Note 23 - Consolidated Fund 52 24. Note 24 - Foreign Loan Revolving Funds 52 25. -
(Ifasina) Willeyi Horn (Coleoptera: Cicindelidae) of Sri Lanka
JoTT COMMUNI C ATION 3(2): 1493-1505 The current occurrence, habitat and historical change in the distribution range of an endemic tiger beetle species Cicindela (Ifasina) willeyi Horn (Coleoptera: Cicindelidae) of Sri Lanka Chandima Dangalle 1, Nirmalie Pallewatta 2 & Alfried Vogler 3 1,2 Department of Zoology, Faculty of Science, University of Colombo, Colombo 03, Sri Lanka 3 Department of Entomology, The Natural History Museum, London SW7 5BD, United Kingdom Email: 1 [email protected] (corresponding author), 2 [email protected], 3 [email protected] Date of publication (online): 26 February 2011 Abstract: The current occurrence, habitat and historical change in distributional range Date of publication (print): 26 February 2011 are studied for an endemic tiger beetle species, Cicindela (Ifasina) willeyi Horn of Sri ISSN 0974-7907 (online) | 0974-7893 (print) Lanka. At present, the species is only recorded from Maha Oya (Dehi Owita) and Handapangoda, and is absent from the locations where it previously occurred. The Editor: K.A. Subramanian current habitat of the species is explained using abiotic environmental factors of the Manuscript details: climate and soil recorded using standard methods. Morphology of the species is Ms # o2501 described by studying specimens using identification keys for the genus and comparing Received 02 July 2010 with specimens available at the National Museum of Colombo, Sri Lanka. The DNA Final received 29 December 2010 barcode of the species is elucidated using the mitochondrial CO1 gene sequence of Finally accepted 05 January 2011 eight specimens of Cicindela (Ifasina) willeyi. The study suggests that Maha Oya (Dehi Owita) and Handapangoda are suitable habitats. -
The Effect of Water Bodies As a Determinant Force in Generating Urban Form
The Effect of Water Bodies as a Determinant Force in Generating Urban Form. A Study on Creating a Symbiosis between the two with a case study of the Beira Lake, City of Colombo. K. Pradeep S. S. Fernando. 139404R Degree of Masters in Urban Design 2016 Department of Architecture University of Moratuwa Sri Lanka The Effect of Water Bodies as a Determinant Force in Generating Urban Form. A Study on Creating a Symbiosis between the two with a case study of the Beira Lake, City of Colombo. K. Pradeep S. S. Fernando. 139404R Degree of Masters in Urban Design 2016 Department of Architecture University of Moratuwa Sri Lanka THE EFFECT OF WATER BODIES AS A DETERMINANT FORCE IN GENERATING URBAN FORM - WITH A STUDY ON CREATING A SYMBIOSIS BETWEEN THE TWO WITH A CASE STUDY OF THE BEIRA LAKE, CITY OF COLOMBO. Water bodies present in Urban Contexts has been a primary determinant force in the urban formation and settlement patterns. With the evolutionary patterns governing the cities, the presence of water bodies has been a primary generator bias, thus being a primary contributor to the character of the city and the urban morphology. Urban form can be perceived as the pattern in which the city is formed where the street patterns and nodes are created, and the 03 dimensional built forms, which holistically forms the urban landscape. The perception of urban form has also been a key factor in the human response to the built massing, and fabric whereby the activity pattern is derived, with the sociological implications. DECLARATION I declare that this my own work and this dissertation does not incorporate without acknowledgment any material previously submitted for a Degree or Diploma in any University or any Institute of Higher Learning and to the best of my knowledge and belief it does not contain any materials previously published or written by another person except where acknowledgement is made in the text. -
Water Balance Variability Across Sri Lanka for Assessing Agricultural and Environmental Water Use W.G.M
Agricultural Water Management 58 (2003) 171±192 Water balance variability across Sri Lanka for assessing agricultural and environmental water use W.G.M. Bastiaanssena,*, L. Chandrapalab aInternational Water Management Institute (IWMI), P.O. Box 2075, Colombo, Sri Lanka bDepartment of Meteorology, 383 Bauddaloka Mawatha, Colombo 7, Sri Lanka Abstract This paper describes a new procedure for hydrological data collection and assessment of agricultural and environmental water use using public domain satellite data. The variability of the annual water balance for Sri Lanka is estimated using observed rainfall and remotely sensed actual evaporation rates at a 1 km grid resolution. The Surface Energy Balance Algorithm for Land (SEBAL) has been used to assess the actual evaporation and storage changes in the root zone on a 10- day basis. The water balance was closed with a runoff component and a remainder term. Evaporation and runoff estimates were veri®ed against ground measurements using scintillometry and gauge readings respectively. The annual water balance for each of the 103 river basins of Sri Lanka is presented. The remainder term appeared to be less than 10% of the rainfall, which implies that the water balance is suf®ciently understood for policy and decision making. Access to water balance data is necessary as input into water accounting procedures, which simply describe the water status in hydrological systems (e.g. nation wide, river basin, irrigation scheme). The results show that the irrigation sector uses not more than 7% of the net water in¯ow. The total agricultural water use and the environmental systems usage is 15 and 51%, respectively of the net water in¯ow. -
River Basins
APPENDIX I.I 122 River Basins Basin No Name of Basin Catchment Basin No. Name of Basin Catchment Area Sq. Km. Area Sq. Km 1. Kelani Ganga 2278 53. Miyangolla Ela 225 2. Bolgoda Lake 374 54. Maduru Oya 1541 3. Kaluganga 2688 55. Pulliyanpotha Aru 52 4. Bemota Ganga 6622 56. Kirimechi Odai 77 5. Madu Ganga 59 57. Bodigoda Aru 164 6. Madampe Lake 90 58. Mandan Aru 13 7. Telwatte Ganga 51 59. Makarachchi Aru 37 8. Ratgama Lake 10 60. Mahaweli Ganga 10327 9. Gin Ganga 922 61. Kantalai Basin Per Ara 445- 10. Koggala Lake 64 62. Panna Oya 69 11. Polwatta Ganga 233 12. Nilwala Ganga 960 63. Palampotta Aru 143 13. Sinimodara Oya 38 64. Pankulam Ara 382 14. Kirama Oya 223 65. Kanchikamban Aru 205 15. Rekawa Oya 755 66. Palakutti A/u 20 16. Uruhokke Oya 348 67. Yan Oya 1520 17. Kachigala Ara 220 68. Mee Oya 90 18. Walawe Ganga 2442 69. Ma Oya 1024 19. Karagan Oya 58 70. Churian A/u 74 20. Malala Oya 399 71. Chavar Aru 31 21. Embilikala Oya 59 72. Palladi Aru 61 22. Kirindi Oya 1165 73. Nay Ara 187 23. Bambawe Ara 79 74. Kodalikallu Aru 74 24. Mahasilawa Oya 13 75. Per Ara 374 25. Butawa Oya 38 76. Pali Aru 84 26. Menik Ganga 1272 27. Katupila Aru 86 77. Muruthapilly Aru 41 28. Kuranda Ara 131 78. Thoravi! Aru 90 29. Namadagas Ara 46 79. Piramenthal Aru 82 30. Karambe Ara 46 80. Nethali Aru 120 31. -
List of Rivers of Sri Lanka
Sl. No Name Length Source Drainage Location of mouth (Mahaweli River 335 km (208 mi) Kotmale Trincomalee 08°27′34″N 81°13′46″E / 8.45944°N 81.22944°E / 8.45944; 81.22944 (Mahaweli River 1 (Malvathu River 164 km (102 mi) Dambulla Vankalai 08°48′08″N 79°55′40″E / 8.80222°N 79.92778°E / 8.80222; 79.92778 (Malvathu River 2 (Kala Oya 148 km (92 mi) Dambulla Wilpattu 08°17′41″N 79°50′23″E / 8.29472°N 79.83972°E / 8.29472; 79.83972 (Kala Oya 3 (Kelani River 145 km (90 mi) Horton Plains Colombo 06°58′44″N 79°52′12″E / 6.97889°N 79.87000°E / 6.97889; 79.87000 (Kelani River 4 (Yan Oya 142 km (88 mi) Ritigala Pulmoddai 08°55′04″N 81°00′58″E / 8.91778°N 81.01611°E / 8.91778; 81.01611 (Yan Oya 5 (Deduru Oya 142 km (88 mi) Kurunegala Chilaw 07°36′50″N 79°48′12″E / 7.61389°N 79.80333°E / 7.61389; 79.80333 (Deduru Oya 6 (Walawe River 138 km (86 mi) Balangoda Ambalantota 06°06′19″N 81°00′57″E / 6.10528°N 81.01583°E / 6.10528; 81.01583 (Walawe River 7 (Maduru Oya 135 km (84 mi) Maduru Oya Kalkudah 07°56′24″N 81°33′05″E / 7.94000°N 81.55139°E / 7.94000; 81.55139 (Maduru Oya 8 (Maha Oya 134 km (83 mi) Hakurugammana Negombo 07°16′21″N 79°50′34″E / 7.27250°N 79.84278°E / 7.27250; 79.84278 (Maha Oya 9 (Kalu Ganga 129 km (80 mi) Adam's Peak Kalutara 06°34′10″N 79°57′44″E / 6.56944°N 79.96222°E / 6.56944; 79.96222 (Kalu Ganga 10 (Kirindi Oya 117 km (73 mi) Bandarawela Bundala 06°11′39″N 81°17′34″E / 6.19417°N 81.29278°E / 6.19417; 81.29278 (Kirindi Oya 11 (Kumbukkan Oya 116 km (72 mi) Dombagahawela Arugam Bay 06°48′36″N -
Securing the Food Supply and Food Security of the Ruhuna Basin
Securing the Food Supply and Food Security of the Ruhuna Basin K. D. N. Weerasinghe\ Ananda Jayasinghe2 and A. M. H. Abeysinghe3 1. Geographical Informations of the Ruhuha Basins Ruhuna basin situates in southern Sri Lanka totaling 5578 sq krn. It has four major river basins viz: Walawe Ganga, Kirindi Oya, Malala Oya and Menik Ganga. There are 3 Agro-ecological zones in the Ruhuna Basin namely Wet, Wet Intermediate and Dry Intermediate zones. Major River Basins of the Ruhuna basin and their catchments are given in the table 1 and figure 1. Table 1. Major river basins and catchments. Name Catchment's area (Km2) 1. Walawe Ganga 2471 2. Kiridi Oya 1165 3. Menik Ganga 1287 4. Malala Oya 402 5. Other 235 Total 5578 Palitha et aI, 1999) Total area of the Ruhuna Basin is c0vered by catchments of Walawe Ganga, Kirindi Oya, Malala Oya, Manik Ganga and number of small catchments. Detailed map of the river basins in the Hambantota District as documented by J. L. Sabatier (2001), is given in the figure 1. There are 19 river basins in the district and out of which 10 river basins are included in to the Ruhuna basin, except, Seenimodera, Kirama, Rekawa,Urubokke Oya, in the west and Katupila Ara, Kurundu Ara, Nemadegan Ara, Karambe Ara, and Kumbukkan Oya in the east (Figure 1). Further more as pointed out by Arumugam (1969), most of these basins are small and they do not make any effective contribution to the water resources. Malala Oya basin has a catchment of 404 sq. -
The Freshwater Fisheries of Ceylon
The freshwater fisheries of Ceylon Item Type article Authors Fernando, C.H.; Indrasena, H.H.A. Download date 01/10/2021 02:57:17 Link to Item http://hdl.handle.net/1834/32569 Bull. Fish. Res. Stn., Ceylon. Vol. 20,No.2, pp. 101-134 Decernbe1·, 1969 The Freshwater Fisheries of Ceylon c. H. FERN.AND0 1 .AND H. H. A. INDR.ASEN.A 2 INTRODUCTION THERE is no comprehensive account of the fresh·water fisheries of Ceylon. The present paper is an attempt at such a treatment. Our task has been somewhat simplified by the paucity of previous work but on the other hand data relevant to the subject is scattered and not easily available in the usual abstracting journals. This paper is based on a collection of data over the last fifteen years while associated with the Fisheries Depa.rtment and information gathered from other agencies concerned with water resources in Ceylon. The authors have added their own work during this period both published and unpublished. The introduction of :Pilapict mossambica Peters into natural waters in Ceylon in HJ51 and its subsequent rapid spread and dominance of the fish catches has had a profound impact on all aspects of freshwater fisheries. The tremendous increase in fish production has been accompanied by changes in fishing methods and improved utilization. On the basis of the experience ·with the introduction of this species other species have been considered for introduction. The expansion of the freshwater area by the construction of irrigation a.nd hydro electric reservoirs has increased the fish production potential considerably during the last fifteen years. -
Y%S ,Xld M%Cd;Dka;%Sl Iudcjd§ Ckrcfha .Eiü M;%H W;S Úfyi the Gazette of the Democratic Socialist Republic of Sri Lanka EXTRAORDINARY
Y%S ,xld m%cd;dka;%sl iudcjd§ ckrcfha .eiÜ m;%h w;s úfYI The Gazette of the Democratic Socialist Republic of Sri Lanka EXTRAORDINARY wxl 2072$58 - 2018 uehs ui 25 jeks isl=rdod - 2018'05'25 No. 2072/58 - FRIDAY, MAY 25, 2018 (Published by Authority) PART I : SECTION (I) — GENERAL Government Notifications SRI LANKA Coastal ZONE AND Coastal RESOURCE MANAGEMENT PLAN - 2018 Prepared under Section 12(1) of the Coast Conservation and Coastal Resource Management Act, No. 57 of 1981 THE Public are hereby informed that the Sri Lanka Coastal Zone and Coastal Resource Management Plan - 2018 was approved by the cabinet of Ministers on 25th April 2018 and the Plan is implemented with effect from the date of Gazette Notification. MAITHRIPALA SIRISENA, Minister of Mahaweli Development and Environment. Ministry of Mahaweli Development and Environment, No. 500, T. B. Jayah Mawatha, Colombo 10, 23rd May, 2018. 1A PG 04054 - 507 (05/2018) This Gazette Extraordinary can be downloaded from www.documents.gov.lk 1A 2A I fldgi ( ^I& fPoh - YS% ,xld m%cd;dka;s%l iudcjd§ ckrcfha w;s úfYI .eiÜ m;%h - 2018'05'25 PART I : SEC. (I) - GAZETTE EXTRAORDINARY OF THE DEMOCRATIC SOCIALIST REPUBLIC OF SRI LANKA - 25.05.2018 CHAPTER 1 1. INTRODUCTION 1.1 THE SCOPE FOR COASTAL ZONE AND COASTAL RESOURCE MANAGEMENT 1.1.1. Context and Setting With the increase of population and accelerated economic activities in the coastal region, the requirement of integrated management focused on conserving, developing and sustainable utilization of Sri Lanka’s dynamic and resources rich coastal region has long been recognized. -
Ancient Water Management and Governance in the Dry Zone of Sri Lanka Until Abandonment, and the Influence of Colonial Politics During Reclamation
water Article Ancient Water Management and Governance in the Dry Zone of Sri Lanka Until Abandonment, and the Influence of Colonial Politics during Reclamation Nuwan Abeywardana * , Wiebke Bebermeier * and Brigitta Schütt Department of Earth Sciences, Physical Geography, Freie Universität Berlin, Malteserstr. 74-100, 12249 Berlin, Germany; [email protected] * Correspondence: [email protected] (N.A.), [email protected] (W.B.) Received: 30 October 2018; Accepted: 21 November 2018; Published: 27 November 2018 Abstract: The dry-zone water-harvesting and management system in Sri Lanka is one of the oldest historically recorded systems in the world. A substantial number of ancient sources mention the management and governance structure of this system suggesting it was initiated in the 4th century BCE (Before Common Era) and abandoned in the middle of the 13th century CE (Common Era). In the 19th century CE, it was reused under the British colonial government. This research aims to identify the ancient water management and governance structure in the dry zone of Sri Lanka through a systematic analysis of ancient sources. Furthermore, colonial politics and interventions during reclamation have been critically analyzed. Information was captured from 222 text passages containing 560 different records. 201 of these text passages were captured from lithic inscriptions and 21 text passages originate from the chronicles. The spatial and temporal distribution of the records and the qualitative information they contain reflect the evolution of the water management and governance systems in Sri Lanka. Vast multitudes of small tanks were developed and managed by the local communities. Due to the sustainable management structure set up within society, the small tank systems have remained intact for more than two millennia.