3 research outputs found

    HIGH PERFORMANCE CMOS WIDE-BAND RF FRONT-END WITH SUBTHRESHOLD OUT OF BAND SENSING

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    In future, the radar/satellite wireless communication devices must support multiple standards and should be designed in the form of system-on-chip (SoC) so that a significant reduction happen on cost, area, pins, and power etc. However, in such device, the design of a fully on-chip CMOS wideband receiver front-end that can process several radar/satellite signal simultaneously becomes a multifold complex problem. Further, the inherent high-power out-of-band (OB) blockers in radio spectrum will make the receiver more non-linear, even sometimes saturate the receiver. Therefore, the proper blocker rejection techniques need to be incorporated. The primary focus of this research work is the development of a CMOS high-performance low noise wideband receiver architecture with a subthreshold out of band sensing receiver. Further, the various reconfigurable mixer architectures are proposed for performance adaptability of a wideband receiver for incoming standards. Firstly, a high-performance low- noise bandwidthenhanced fully differential receiver is proposed. The receiver composed of a composite transistor pair noise canceled low noise amplifier (LNA), multi-gate-transistor (MGTR) trans-conductor amplifier, and passive switching quad followed by Tow Thomas bi-quad second order filter based tarns-impedance amplifier. An inductive degenerative technique with low-VT CMOS architecture in LNA helps to improve the bandwidth and noise figure of the receiver. The full receiver system is designed in UMC 65nm CMOS technology and measured. The packaged LNA provides a power gain 12dB (including buffer) with a 3dB bandwidth of 0.3G – 3G, noise figure of 1.8 dB having a power consumption of 18.75mW with an active area of 1.2mm*1mm. The measured receiver shows 37dB gain at 5MHz IF frequency with 1.85dB noise figure and IIP3 of +6dBm, occupies 2mm*1.2mm area with 44.5mW of power consumption. Secondly, a 3GHz-5GHz auxiliary subthreshold receiver is proposed to estimate the out of blocker power. As a redundant block in the system, the cost and power minimization of the auxiliary receiver are achieved via subthreshold circuit design techniques and implementing the design in higher technology node (180nm CMOS). The packaged auxiliary receiver gives a voltage gain of 20dB gain, the noise figure of 8.9dB noise figure, IIP3 of -10dBm and 2G-5GHz bandwidth with 3.02mW power consumption. As per the knowledge, the measured results of proposed main-high-performancereceiver and auxiliary-subthreshold-receiver are best in state of art design. Finally, the various viii reconfigurable mixers architectures are proposed to reconfigure the main-receiver performance according to the requirement of the selected communication standard. The down conversion mixers configurability are in the form of active/passive and Input (RF) and output (IF) bandwidth reconfigurability. All designs are simulated in 65nm CMOS technology. To validate the concept, the active/ passive reconfigurable mixer configuration is fabricated and measured. Measured result shows a conversion gain of 29.2 dB and 25.5 dB, noise figure of 7.7 dB and 10.2 dB, IIP3 of -11.9 dBm and 6.5 dBm in active and passive mode respectively. It consumes a power 9.24mW and 9.36mW in passive and active case with a bandwidth of 1 to 5.5 GHz and 0.5 to 5.1 GHz for active/passive case respectively

    A 1.2V, 2.7mA Receiver Front-End for Bluetooth Low Energy Applications

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    The Core Project Biospheric Aspects of the Hydrological Cycle (BAHC) of the International Geosphere Biosphere Programme (IGBP) addresses the biospheric aspects of the hydrological cycle through experiments and modelling of energy, water, carbon dioxide and sediment fluxes in the soil-vegetation-atmosphere system at a variety of spatial and temporal scales. Active regulation of water, energy and carbon dioxide fluxes by the vegetation make it an important factor in regulating the Earth's hydrological cycle and in the formation of the climate. Consequently, human induced conversion of vegetation cover is an important driver for climate change. A number of recent studies, discussed in this paper, emphasise the importance of the terrestrial biosphere for the climate system. Initially, these studies demonstrate the influence of the land surface on tropical weather and climate, revealing the mechanisms, acting at various scales, that connect increasing temperatures and decreasing rainfall to large-scale deforestation and other forms of land degradation. More recently, the significance of the land surface processes for water cycle and for weather and climate in temperate and boreal zones was demonstrated. In addition the terrestrial biosphere plays a significant role in the carbon dioxide fluxes and in global carbon balance. Recent work suggests that many ecosystems both in the tropics and in temperate zones may act as a substantial sink for carbon dioxide, though the temporal variability of this sink strength is yet unclear. Further, carbon dioxide uptake and evaporation by vegetation are intrinsically coupled leading to Links and feedbacks between land surface and climate that are hardly explored yet. Earth's vegetation cover and its changes owing to human impact have a profound influence on a lateral redistribution of water and transported constituents, such as nutrients and sediments, and acts therefore as an important moderator of Earth's biogeochemical cycles. In the BAHC science programme, the importance of studying the influence of climate and human activities on mobilisation and river-borne transport of constituents is explicitly articulated. The terrestrial water and associated material cycles are studied as highly dynamic in space and time, and reflect a complex interplay among climatic forcing, topography, land cover and vegetation dynamics. Despite a large progress in our understanding of how the terrestrial biosphere interacts with Earth's and climate system and with the terrestrial part of its hydrological cycle, a number of basic issues still remain unresolved. Limited to the scope of BAHC, the paper briefly assesses the present status and identifies the most important outstanding issues, which require further research. Two, arguably most important outstanding issues are identified: a limited understanding of natural variability, especially with respect to seasonal to inter-annual cycles, and of a complex ecosystem behaviour resulting from multiple feedbacks and multiple coupled biogeochemical cycles within the overall climate system. This leads to two major challenges for the future science agenda related to global change research. First, there is a need for a strong multidisciplinary integration of research efforts in both modelling and experiments, the latter extending to inter-annual timescales. Second, the ever increasing complexity in characterisation and modelling of the climate system, which is mainly owing to incorporation of the biosphere's and human feedbacks, may call for a new approach in global change impact studies. Methodologies need to be developed to identify risks to, and vulnerability of environmental systems, taking into account all important interactions between atmospheric, ecological and hydrological processes at relevant scales. With respect to the influence of climate and human activities on mobilisation and river-borne transport of constituents, the main issues for the future are related to declining availability and quality of ground data for quantity and quality of water discharge. Such assessments presented in this paper, in combination with community wide science evaluation, has lead to an update of the science agenda for BAHC, a summary of which is provided in the appendix. (C) 1998 Elsevier Science B.V. All rights reserved. [References: 97
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