巴尔喀什湖是居里海和地球上干涸的阿拉尔内陆湖之后的第三大湖，它位于中亚干旱地区，哈萨克斯坦的东南部。巴尔喀什湖面积为413000平方千米，其中有113000平方千米，或超过27%的面积在中国新疆维吾尔自治区的领域上。伊犁河是外巴尔喀什湖主要的水源，伊犁河保证80%的干净河水流入巴尔喀什湖。每年恢复的水资源（地表水）形成地带主要位于中国的新疆维吾尔自治区，所以超过60%的伊犁河水径流进入相邻地区的湖中。 提供的专著专供伊犁-巴尔喀什湖流域现代生态状况的评估。\n本书由10个章节组成。第一章提供了巴尔喀什湖流域自然条件的总描述；第二章提供了伊犁-巴尔喀什湖流域经济领域的分析结果：第三章和第四章提供了巴尔喀什湖，伊犁河三角洲和卡普恰盖水库的鱼类区系状态的深入分析；第五章详细描写了伊犁-巴尔喀什湖流域的哈萨克斯坦地区外伊犁山脉冰川的现代状况；第六章提供了巴尔喀什湖流域地下水状况的公正和客观的评价； 第七和第八章展示了巴尔喀什湖、伊犁河三角洲的相互影响，描写了三角洲小支流的河床演变过程，其水资源的发展和开支阶段取决于这些阶段。第九章提供了巴尔喀什湖流域植物的现状，包括在平原和伊犁河三角洲的高山森林，山麓草原，沙地高原。对植物群落状况进行了评估；第十章对南外巴尔喀什湖的沙地高原的风蚀过程进行了评估。
", "ds_source": "由阿拉木图卡加那特出版社2002年出版的《巴尔喀什湖流域现代生态状况》，地质矿物学副教授T.K库然科娃审定，俄文原版图书。
", "ds_process_way": "先对原著图书进行高分辨率扫描（300dpi)，然后聘请俄文专业翻译对原文进行中文翻译。
", "ds_quality": "翻译中对文字部分进行生态学的专业校订，文中数据没有删减改动，遵照原文。
", "ds_acq_start_time": "2002-01-01 00:00:00", "ds_acq_end_time": null, "ds_acq_place": "哈萨克斯坦", "ds_acq_lon_east": null, "ds_acq_lat_south": null, "ds_acq_lon_west": null, "ds_acq_lat_north": null, "ds_acq_alt_low": null, "ds_acq_alt_high": null, "ds_share_type": "login-access", "ds_total_size": 104153322, "ds_files_count": 3, "ds_format": "doc", "ds_space_res": null, "ds_time_res": "年", "ds_coordinate": "无", "ds_projection": "", "ds_thumbnail": "ee694591-29bc-44d2-a8d1-8f3fb813dd5b.jpg", "ds_thumb_from": 0, "ds_ref_way": "", "paper_ref_way": "", "ds_ref_instruction": "在使用数据时，请注明“巴尔喀什湖流域现代生态状况(2002年）数据来自中科院新疆生态与地理研究所”", "ds_from_station": null, "organization_id": "52b7b79b-860c-49a5-9083-9a70cf8bed5a", "ds_serv_man": "李锦", "ds_serv_phone": "09917827369", "ds_serv_mail": "lijin@ms.xjb.ac.cn", "doi_value": "", "subject_codes": [ "170.4510" ], "quality_level": 3, "publish_time": "2020-04-09 10:11:08", "last_updated": "2023-08-25 10:51:42", "protected": false, "protected_to": null, "lang": "zh", "cstr": "11738.11.ncdc.nieer.2020.1389", "i18n": { "en": { "title": "The modern ecological situation of barkash Lake Basin", "ds_format": "doc", "ds_source": "The modern ecological situation of balkashi Lake Basin published by Almaty kaganat press in 2002, approved by T.K. kurankova, associate professor of Geology and mineralogy, and the original Russian book.
", "ds_quality": "In the translation, there is a professional revision of the text in terms of ecology, and the data in the text has not been deleted or modified, following the original text
", "ds_ref_way": "", "ds_abstract": "Barkash lake is the third largest lake after the Curie sea and the dry alar inland lake on earth. It is located in the arid area of Central Asia, Southeast of Kazakhstan. Balkhash Lake covers an area of 413000 square kilometers, including 113000 square kilometers, or more than 27% of the area in Xinjiang Uygur Autonomous Region of China. Ili River is the main source of water for outer balkashi lake. Ili River ensures 80% of the clean water flows into balkashi lake. The water resources (surface water) formation area recovered every year is mainly located in Xinjiang Uygur Autonomous Region of China, so more than 60% of the Yili River Runoff flows into the adjacent lakes. The monograph provided is dedicated to the assessment of modern ecological conditions in Ili - barkash Lake Basin.\n
The book consists of 10 chapters. The first chapter provides a general description of the natural conditions of the balkashi Lake Basin; the second chapter provides the results of the economic analysis of the Ili balkashi Lake Basin; the third and fourth chapters provide an in-depth analysis of the fish fauna of the balkashi lake, the Ili River Delta and the kapchagai reservoir; the fifth chapter describes in detail the areas outside Kazakhstan of the Ili balkashi Lake Basin The sixth chapter provides a fair and objective evaluation of groundwater conditions in the balkashi Lake Basin; the seventh and eighth chapters show the interaction between the balkashi lake and the Ili River Delta, and describe the river bed evolution process of small tributaries in the delta. The development and expenditure stages of water resources depend on these stages. Chapter 9 provides the current situation of plants in balkashi Lake Basin, including alpine forest, piedmont grassland and sandy plateau in plain and Ili River Delta. In Chapter 10, the process of wind erosion in the sandy plateau of barkash lake, South China, is evaluated.
\n", "ds_time_res": "年", "ds_acq_place": "Kazakhstan", "ds_space_res": "", "ds_projection": "", "ds_process_way": "First, the original books were scanned with high resolution (300dpi), and then the Russian professional translator was employed to translate the original Chinese.
", "ds_ref_instruction": "When using the data, please indicate that \"the data of the modern ecological situation of the barkash Lake Basin (2002) is from Xinjiang Institute of ecology and geography, Chinese Academy of Sciences\"" } }, "submit_center_id": "ncdc", "data_level": 0, "license_type": "CC BY 4.0", "doi_reg_from": "reg_local", "cstr_reg_from": "reg_local", "doi_not_reg_reason": null, "cstr_not_reg_reason": null, "is_paper_in_submitting": false, "ds_topic_tags": [ "生态", "流域水问题", "巴尔喀什湖", "跨国界河流" ], "ds_subject_tags": [ "自然地理学" ], "ds_class_tags": [], "ds_locus_tags": [ "额尔齐斯河", "哈萨克斯坦" ], "ds_time_tags": [ 2002 ], "ds_contributors": [ { "true_name": "吴淼", "email": "wumiao@ms.xjb.ac.cn", "work_for": "中国科学院新疆生态与地理研究所文献信息中心", "country": "中国" } ], "ds_meta_authors": [ { "true_name": "李锦", "email": "lijin@ms.xjb.ac.cn", "work_for": "新疆生态与地理研究所", "country": "中国" } ], "ds_managers": [ { "true_name": "李锦", "email": "lijin@ms.xjb.ac.cn", "work_for": "新疆生态与地理研究所", "country": "中国" }, { "true_name": "吴淼", "email": "wumiao@ms.xjb.ac.cn", "work_for": "中国科学院新疆生态与地理研究所文献信息中心", "country": "中国" } ], "category": "生态" }