The reclamation of abondend open-cast mines in the region south of Leipzig raises many scientific questions. This research project focus on the simulation of groundwater recharge. The knowledge of the processes of water infiltration is necessary to control the recharge and quality of groundwater. Empirical and mathematical methods will be combined to estimate the groundwater recharge according to substrate, vegetation and landuse. For this purpose on the open-cast mine Espenhain two soil long-term observation stations under different landuse conditions (forest, agricultural area) were installed. The following parameters are measured in different levels up to 2 m depth continuously every 30 minutes: Soil water content, water tension, soil temperature. On the forest station stem flow and precipitation are determined. On the agricultural area open land precipitation, air temperature, air humidity and albedo are registered automatically. Soil water and rainfall are analyzed on heavy metal contents as well as different cations and anions. Parallel to the field measurements on the institute workstation the computer model WASMOD was used for long-term predictions of groundwater recharge. The WASMOD model is calibrated with the measured data of the observation stations and coupled with a geographical information system in order to obtain groundwater recharge for the Espenhain dump.

With an abundant average precipitation rate, Vietnam could be considered water-reach country. Unfortunately, the non-uniform spatial and temporal distribution of rainfall, coupled with a demographic and industrial development polarized on the two major river deltas, it makes the water resources extremely vulnerable. As consequence, severe depletions of groundwater table are reported all over the country, often in the range of 1-2 m per year and more. The subsequent land subsidence is just one of the drawbacks, another being the increasing salinity of coastal aquifers as sea water level continues to rise. Under these conditions, the natural groundwater replenishment alone is not anymore able to provide for a safe water supply, different studies indicating that the groundwater exploitation in major urban agglomerations like Hanoi or Ho Chi Minh City already passed the sustainability level. The solution presented in this paper implies making use of engineered methods for enhancing the natural groundwater recharge rates by enabling better percolation rates of surface water into subsurface and thus optimizing the regional water cycle. The method known as ‘managed aquifer recharge’ (MAR) is introduced, together with general guidelines and tools for planning of MAR schemes, such as the newly web-based decision support system INOWAS_DSS. / Với tốc độ lượng mưa trung bình dồi dào, Việt Nam có thể được coi là quốc gia có nguồn nước trong tầm tay. Thật không may, sự phân bố không gian và thời gian không đồng đều của lượng mưa, cùng với sự phát triển dân số và công nghiệp phân cực trên hai vùng châu thổ sông lớn làm cho các nguồn nước rất dễ bị tổn thương. Vì vậy, sự suy giảm nước ngầm nghiêm trọng được báo cáo trên khắp đất nước, thường mỗi năm giảm 1-2 m và nhiều hơn nữa. Hiện tượng sụt lún đất xảy ra sau đó chỉ là một trong những hạn chế, mặt khác là độ mặn ngày càng tăng của các tầng chứa nước ven biển do mực nước biển tiếp tục tăng. Dưới những điều kiện này, việc bổ sung nước ngầm tự nhiên đơn thuần không còn có thể cung ứng cho một nguồn cấp nước sạch an toàn. Các nghiên cứu khác nhau cho thấy rằng việc khai thác nước ngầm tại các đô thị lớn như Hà Nội hay thành phố Hồ Chí Minh đã vượt qua mức độ bền vững. Giải pháp được trình bày trong bài báo này gợi ý việc sử dụng các phương pháp thiết kế để nâng cao tỷ lệ tái nạp nước ngầm tự nhiên bằng cách cho phép tỷ lệ thẩm thấu tốt hơn nước mặt vào dưới bề mặt và do đó tối ưu hóa chu trình nước trong khu vực. Phương pháp được gọi là 'tái nạp nước ngầm có quản lý (MAR) được giới thiệu, cùng với các hướng dẫn chung và các công cụ để lập kế hoạch đề án MAR, ví dụ như hệ thống mớihỗ trợ quyết định dựa trên kết nối mạng INOWAS_DSS.

The reclamation of abondend open-cast mines in the region south of Leipzig raises many scientific questions. This research project focus on the simulation of groundwater recharge. The knowledge of the processes of water infiltration is necessary to control the recharge and quality of groundwater. Empirical and mathematical methods will be combined to estimate the groundwater recharge according to substrate, vegetation and landuse. For this purpose on the open-cast mine Espenhain two soil long-term observation stations under different landuse conditions (forest, agricultural area) were installed. The following parameters are measured in different levels up to 2 m depth continuously every 30 minutes: Soil water content, water tension, soil temperature. On the forest station stem flow and precipitation are determined. On the agricultural area open land precipitation, air temperature, air humidity and albedo are registered automatically. Soil water and rainfall are analyzed on heavy metal contents as well as different cations and anions. Parallel to the field measurements on the institute workstation the computer model WASMOD was used for long-term predictions of groundwater recharge. The WASMOD model is calibrated with the measured data of the observation stations and coupled with a geographical information system in order to obtain groundwater recharge for the Espenhain dump.

Die Bewirtschaftung der knappen Ressource sauberen Wassers setzt das Verständnis der Wasserhaushaltsprozesse voraus. Mit prozessorientierten Modellen können Wasserbilanzen für unterschiedliche Standortbedingungen berechnet werden, wenn die Modelle zuvor an repräsentativen Zeitreihen, die die notwendige hydrologische Information enthalten, kalibriert und die Sensitivität ihrer Parameter analysiert wurden. Am Groß-Lysimeter St. Arnold (Westfalen) werden seit 1966 neben den meteorologischen Parametern tägliche Sickerwasserraten gemessen, die für diesen Zweck hervorragend geeignet sind, weil sie integrale Bilanzgrößen über die je 400m² x 3,50m großen Podsol-Bodenkörper und ihre Vegetationsbestände darstellen. Auf den drei Lysimetern wachsen Gras, ein Eichen-/Buchen- bzw. ein Kiefernbestand. Für die Untersuchung der Wasserhaushaltsprozesse wird das "LYsimeter outFlow and Evapotranspiration model" LYFE, entwickelt. Es verknüpft die Richards-Gleichung mit einem Interzeptionsmodell, das den Niederschlag in Infiltration, Blatt- und Streuinterzeption aufspaltet. Die Evapotranspirations-(ET)-Raten werden alternativ mit der Penman- oder Monteith-Formel berechnet. Die Simulationen vollziehen die gemessenen täglichen Sickerwasserraten aller drei Lysimeter unter den Klimavariabilitäten des gesamten Zeitraums von 34 Jahren nach. Am Graslysimeter ist die Sensitivität der ET-Parameter gering, so dass unterschiedlich aufwendige Methoden zur Bestimmung der bodenhydraulischen Parameter verglichen und bewertet werden können: die statischen Stechzylindermessungen der Retention und gesättigten Leitfähigkeit, der Verdunstungsversuch und verschiedene Pedotransferfunktionen (PTF). Die Simulation mit den Parametern des Verdunstungsversuchs ergeben eine gute Übereinstimmung mit den gemessenen Sickerwasserraten, während die Parameter der statischen Messungen durch die inverse Modellierung mindestens eines Parameters angepasst werden müssen. Von den PTF erzielen die kontinuierliche und die Klassen-PTF von Wösten die besten Übereinstimmungen. Der Wasserhaushalt der Baumbestände wird von der Interzeption dominiert. Dies gilt insbesondere für die Interzeptionsverdunstung im Winterhalbjahr, die die Unterschiedlichkeit der Wasserbilanz von Laub- und Nadelbaumbeständen verursacht. Wenn die ET mit der Penman-Formel berechnet wird, können die Raten der Evaporation und Transpiration nur schlecht abgeschätzt werden und steigen nicht mit dem Wachstum der Bestände. Durch die Verwendung der Monteith-Formel werden diese Probleme behoben. Darüberhinaus zeigt das Modell die unterschiedliche Wirkung von Transpiration und Interzeptionsverdunstung auf den Jahresgang der Sickerwasserraten und ermöglicht so die Angabe ihrer jeweiligen Beiträge zum Wasserhaushalt. Mit dem kalibrierten Modell können die lysimetrischen Messungen auf andere Standorte übertragen werden, um die langfristige Wasserbilanz zeitlich hochaufgelöst zu bestimmen. Daher kann LYFE im Rahmen regionaler Wasserhaushaltsuntersuchungen eingesetzt werden.

With an abundant average precipitation rate, Vietnam could be considered water-reach country. Unfortunately, the non-uniform spatial and temporal distribution of rainfall, coupled with a demographic and industrial development polarized on the two major river deltas, it makes the water resources extremely vulnerable. As consequence, severe depletions of groundwater table are reported all over the country, often in the range of 1-2 m per year and more. The subsequent land subsidence is just one of the drawbacks, another being the increasing salinity of coastal aquifers as sea water level continues to rise. Under these conditions, the natural groundwater replenishment alone is not anymore able to provide for a safe water supply, different studies indicating that the groundwater exploitation in major urban agglomerations like Hanoi or Ho Chi Minh City already passed the sustainability level. The solution presented in this paper implies making use of engineered methods for enhancing the natural groundwater recharge rates by enabling better percolation rates of surface water into subsurface and thus optimizing the regional water cycle. The method known as ‘managed aquifer recharge’ (MAR) is introduced, together with general guidelines and tools for planning of MAR schemes, such as the newly web-based decision support system INOWAS_DSS. / Với tốc độ lượng mưa trung bình dồi dào, Việt Nam có thể được coi là quốc gia có nguồn nước trong tầm tay. Thật không may, sự phân bố không gian và thời gian không đồng đều của lượng mưa, cùng với sự phát triển dân số và công nghiệp phân cực trên hai vùng châu thổ sông lớn làm cho các nguồn nước rất dễ bị tổn thương. Vì vậy, sự suy giảm nước ngầm nghiêm trọng được báo cáo trên khắp đất nước, thường mỗi năm giảm 1-2 m và nhiều hơn nữa. Hiện tượng sụt lún đất xảy ra sau đó chỉ là một trong những hạn chế, mặt khác là độ mặn ngày càng tăng của các tầng chứa nước ven biển do mực nước biển tiếp tục tăng. Dưới những điều kiện này, việc bổ sung nước ngầm tự nhiên đơn thuần không còn có thể cung ứng cho một nguồn cấp nước sạch an toàn. Các nghiên cứu khác nhau cho thấy rằng việc khai thác nước ngầm tại các đô thị lớn như Hà Nội hay thành phố Hồ Chí Minh đã vượt qua mức độ bền vững. Giải pháp được trình bày trong bài báo này gợi ý việc sử dụng các phương pháp thiết kế để nâng cao tỷ lệ tái nạp nước ngầm tự nhiên bằng cách cho phép tỷ lệ thẩm thấu tốt hơn nước mặt vào dưới bề mặt và do đó tối ưu hóa chu trình nước trong khu vực. Phương pháp được gọi là 'tái nạp nước ngầm có quản lý (MAR) được giới thiệu, cùng với các hướng dẫn chung và các công cụ để lập kế hoạch đề án MAR, ví dụ như hệ thống mớihỗ trợ quyết định dựa trên kết nối mạng INOWAS_DSS.

In den letzten drei Jahrzehnten wurden in einigen Seen und Feuchtgebieten in bewaldeten Einzugsgebieten Nordost-Brandenburgs sinkende Wasserstände beobachtet. In diesen Gebieten bestimmt die Grundwasserneubildung im Einzugsgebiet maßgeblich das Wasserdargebot der Seen und Feuchtgebiete, die deshalb hier als grundwasserabhängige Landschaftselemente bezeichnet werden. Somit weisen die sinkenden Wasserstände auf einen Rückgang der wegen des geringen Niederschlagsdargebotes ohnehin schon geringen Grundwasserneubildung hin. Die Höhe der Grundwasserneubildung ist neben den hydroklimatischen Randbedingungen auch von der Landnutzung abhängig. Veränderungen in der Waldvegetation und der hydroklimatischen Randbedingungen bewirken Änderungen der Grundwasserneubildung und beeinflussen somit auch den Wasserhaushalt der Seen und Feuchtgebiete. Aktuell wird die Waldvegetation durch Kiefernmonokulturen dominiert, mit im Vergleich zu anderen Baumarten höherer Evapotranspiration. Entwicklungen in der Forstwirtschaft streben die Verringerung von Kiefernmonokulturen an. Diese sollen langfristig auf geeigneten Standorten durch Laubmischwälder ersetzt werden. Dadurch lassen sich eine geringere Evapotranspiration und damit eine höhere Grundwasserneubildung erreichen. In der vorliegenden Arbeit werden am Beispiel des Redernswalder Sees und des Briesensees die Ursachen der beobachteten sinkenden Wasserstände analysiert. Ihre Wasserstände nahmen in den letzten 25 Jahren um mehr als 3 Meter ab. Weiterhin wird untersucht, wie die erwarteten Klimaänderungen und Veränderungen in der Waldbewirtschaftung die zukünftige Grundwasserneubildung und den Wasserhaushalt von Seen beeinflussen können. Die Entwicklung der Grundwasserneubildung im Untersuchungsgebiet wurde mit dem Wasserhaushaltsmodell WaSiM-ETH simuliert. Die Analyse der Wechselwirkungen der Seen mit dem regionalen quartären Grundwasserleitersystem erfolgte mit dem 3D-Grundwassermodell FEFLOW. Mögliche zukünftige Veränderungen der Grundwasserneubildung und der Seewasserstände durch Klimaänderungen und Waldumbau wurden mit Szenarienrechnungen bis zum Jahr 2100 analysiert. Die modellgestützte Analyse zeigte, dass die beobachteten abnehmenden Wasserstände zu etwa gleichen Anteilen durch Veränderungen der hydroklimatischen Randbedingungen sowie durch Veränderungen in der Waldvegetation und damit abnehmenden Grundwasserneubildungsraten zu erklären sind. Die zukünftigen Entwicklungen der Grundwasserneubildung und der Wasserstände sind geprägt von sich ändernden hydroklimatischen Randbedingungen und einem sukzessiven Wandel der Kiefernbestände zu Laubwäldern. Der Waldumbau hat positive Wirkungen auf die Grundwasserneubildung und damit auf die Wasserstände. Damit können die Einflüsse des eingesetzten REMO-A1B-Klimaszenarios zum Ende des Modellzeitraumes durch den Waldumbau nicht kompensiert werden, das Sinken des Wasserstandes wird jedoch wesentlich reduziert. Bei dem moderateren REMO-B1-Klimaszenario werden die Wasserstände des Jahres 2008 durch den Waldumbau bis zum Jahr 2100 überschritten. / Declining water levels have been observed in some lakes and wetlands in forested catchments in North-East Brandenburg (Germany). Groundwater recharge mainly controls the supply of water available for lakes and wetlands, therefore determining them as groundwater-dependent landscape elements. Thus, the declining water levels indicate a reduction of groundwater recharge. Aspects such as climate change and different forest management practices have been considered as main factors affecting the regional groundwater regime. Currently, forest landscapes in North-East Brandenburg are dominated by pine monoculture. Depending on the climate conditions, groundwater recharge can be significantly lower under pine than under broad-leaved species like beech or oak. Regional forest administration is currently planning to expand the share of broad-leaved trees among mixed deciduous forest in the future. For this study, two lakes were chosen, the Redernswalder See and the Briesensee at Poratz. Water gauge measurements over the last 25 years showed a decline in lake water level by more than 3 m. To identify and quantify the share of changes in both, climate and forest management, the principal processes were evaluated using field measurements and water balance modelling. In the following step, alternative climate change and forestry scenarios were analysed to discover their impacts on the regional distribution of groundwater recharge. At first, the causes of the declining observed water levels were analysed. For this purpose, the physically based and fully distributed water balance model WaSiM-ETH was used to simulate groundwater recharge in the catchment and evaporation from the lake surfaces from 1958 to 2007. To analyse the geohydrological conditions, a FEFLOW 3D groundwater model was built up for the underlying Quaternary aquifer system. Possible development directions of the water balance were simulated under the influence of climate change and forest conversion until 2100. The model based analysis showed that the observed declining water levels are caused by both changes in climatic boundary conditions and in forest vegetation (age distribution and understorey) followed by decreasing groundwater recharge with an equal magnitude. The future developments of groundwater recharge and water levels are governed by changes in climatic boundary conditions and a transition from pine monoculture to broad-leaved trees. Forest conversion will show a positive effect on groundwater recharge and likely increase the water levels of lakes and wetlands. The forest conversation can not completely compensate the impact of climate change to the lake water levels, but the decrease can be significantly limited.

Deteriorating water quality in the face of a rising demand for agricultural products triggered interest in the groundwater resources of the Najd dessert, an arid region of southern Oman. Groundwater in this area usually is abstracted from one of the largest aquifers on the Arabian Peninsula, the Umm Er Radhuma aquifer. Increased discharge stands in contrast to limited precipitation: the monsoon is an annual event but it is regionally limited; cyclones infrequently occur within the range of three to seven years. Both are possible sources for groundwater recharge in the Najd. With these preconditions in mind, the present study investigates recharge to the Najd groundwaters as part of an active flow system and evaluates the mean residence time in the deep groundwaters. The tools of choice are a groundwater flow model combined with environmental isotope tracer data. The two-dimensional flow model replicates the characteristics of the aquifer system from the potential recharge area in the south (Dhofar Mountains) to the discharge area in the north (Sabkha Umm as Sammim). The south-to-north gradients and the observed artesian heads in the confined aquifer are reproduced. Simulation results indicate that changes between wet and dry periods caused transient responses in heads and head gradients lasting for several thousand years. Based on the used parameters the model calibration indicated, that a recharge rate of around 4 mm a−1 is sufficient to reproduce current groundwater levels. Since rising groundwater levels were documented after cyclone Keila in November 2011, modern recharge evidently occurs. 36-Cl concentrations and dissolved-helium concentrations indicate that the deep groundwaters in the central Najd are up to 550,000 years old. Thus, radiocarbon values indicating groundwater residence times for the central Najd up to 20,000 years and the northern Najd up to 35,000 years underestimate the groundwater residence times and seem to have been strongly affected by mixing during sampling. Decreasing 36-Cl and increasing 4-He concentrations confirm the expected trend in the direction of groundwater flow and prove to be more robust tracers for age dating of Najd groundwaters. Backward pathline tracking was used to simulate the groundwater ages. The tracking results show that a total porosity value between 15 and 20 % is consistent with the range of the observed chlorine-36 and heliumbased ages. The results and parameters obtained in the present study provide the basis for future 3D-groundwater models designed to evaluate the water resources available to the Najd’s agricultural complex. In addition, the developed 2D-model allows for studies of paleoclimate scenarios and their influence on the groundwater regime. / Ein steigender Bedarf nach landwirtschaftlichen Produkten - und damit Wasser - bei gleichzeitiger Abnahme des verfügbaren Wassers in Qualität und Menge in den bisherigen Anbaugebieten, führt zu einer intensiven Nutzung der Grundwasserressourcen der ariden Najd-Region in der Provinz Dhofar, im Süden des Sultanats Oman. Als Quelle dienen die Grundwasservorräte des Umm Er Radhuma-Aquifers, einer der Hauptaquifere auf der arabischen Halbinsel. Der steigenden Nutzung stehen mit dem jährlichen Monsoon, der regional limitiert ist, und unrgelmässigen, zwischen 3 und 7 Jahren auftretenden Unwettern (Zyklonniederschlag) nur begrenzte Niederschlagsmengen als Quellen für eine mögliche Zufuhr von Wasser (Grundwasserneubildung) zum Aquifersystem gegenüber. Der Ansatz der vorliegenden Arbeit besteht darin, mit Hilfe eines Grundwassermodells und der Einbeziehung von Umweltisotopen das tiefe und zur Nutzung geförderte Grundwasser in der Najd-Region als Teil eines aktiven Fließsystemes zu untersuchen und mittlere Verweilzeiten des Grundwassers abzuleiten. Ein 2D-Grundwassermodell entlang einer Fließlinie vom Dhofar Gebirge im Süden zur Sabkha Umm as Sammim im Nordosten wurde entwickelt. Das Modell reproduziert den Süd-Nord-Gradienten als auch den aufwärts gerichteten Gradienten mit höheren Grundwasserständen in den tiefen Grundwasserleitern. Die Simulationen zeigen, dass der Wechsel von ariden und humiden Phasen (wenig bzw. viel Grundwasserneubildung) zu Veränderungen der Grundwasseroberfläche führt die mehrere tausend Jahre anhalten können. Das kalibrierte Grundwassermodel zeigt, dass mit einer Neubildungsrate von 4 mm a−1 die natürlichen Grundwasserverhältnisse im Najd abgebildet werden können. Dass eine moderne Grundwasserneubildung stattfindet, konnte mittels Loggermessungen anhand steigender Grundwasserstände im tiefen Aquifersystem nach dem Extremunwetter im November 2011 (Zyklon Keila) eindeutig nachgewiesen werden. Die Analyse der 36Cl- und 4He-Konzentrationen zeigt, dass die tiefen Grundwasser im zentralen Najdgebiet bis 550 000 Jahren alt sein können. Das bedeutet allerdings, dass die über 14C Daten berechneten Grundwasseralter mit ca. 20 000 Jahren für das zentrale Najdgebiet und bis zu 35 000 Jahren für den nördlichen Najd, die Grundwasseralter deutlich unterschätzen. Die abnehmenden 36Cl und ansteigenden 4He Konzentrationen zeigen den erwarteten Trend in Grundwasserfließrichtung und können als aussagefähige Tracer für die Bewertung der Verweilzeiten und Alter des fossilen Grundwassers der Najd-Region angesehen werden. Mit Hilfe des Partickeltrackings wurden die Grundwasseralter, basierend auf den Isotopentracern, im Grundwassermodel simuliert. Die Porosität wurde dabei für das Aquifesystem mit Werten zwischen 15 und 20 % bestimmt. Die generierten Parameter und das gewonnene Systemverständnis sind eine wichtige Basis für zukünftige 3D-Modellstudien welche die Verfügbarkeit der Wasserresourcen im Najd untersuchen werden. Weitere Anwendungen für das in dieser Studie aufgebaute 2D-Modell sind Untersuchungen zum Paläoklima und dessen Einfluss auf das Grundwassersystem.

No description available.

No description available.

Groundwater is the only fresh water resource in the semi-arid to hyper-arid Western Dead Sea catchment. Due to exploitation of groundwater the water level is decreasing in the surrounding Cretaceous aquifer system and sustainable water management is needed in order to prevent the progressive yields and contamination of those water resources. In addition, the water level of the Dead Sea decreases dramatically by at least one meter per year. This is connected to channel off the water from the Jordan River to supply intensive agriculture in the semi-arid to hyper-arid region. Hydrological and hydro-geological analysis and modelling in arid regions, like the study area, frequently suffer from data scarcity and uncertainties regarding rainfall and discharge measurements. The study showed that spatial and temporal interpolations as well as additional methods (e.g. empirical relationships and simultaneous numerical approaches) were suitable tools to overcome data shortage for modelling. Water balances are the result of a calibrated model and are the basis for sustainable management of surface and subsurface water resources. The present study investigates beside the hydrological characterisation of selected sub-catchments (wadis) also the hydro-geology of the Judean limestone aquifer and calculates a comprehensive water balance of the entire western flank of the Dead Sea by the application of two numerical open source codes: OpenGeoSys (OGS) and J2000g. The calibrated two-dimensional hydrological model J2000g provides a 33 years time series of temporal and spatial distributed groundwater recharge for the numerical groundwater flow model of OGS. The mean annual groundwater recharge of 139.9 · 10^6 m^3ˑ a^-1 is nearly completely depleted by abstractions from pumping wells close to the replenishment area in the Judea Mountains.