Evaluation of the groundnut model PNUTGRO for crop response to water availability, sowing dates, and seasons
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Cited by (43)
Evaluation of the CROPGRO-Peanut model in simulating appropriate sowing date and phosphorus fertilizer application rate for peanut in a subtropical region of eastern India
2017, Crop JournalCitation Excerpt :An alternative approach is to use validated crop growth models and historical climatic data to evaluate various crop management strategies for locations or regions on a long-term basis. To meet these objectives, peanut crop models have been developed in the U.S. [10,11,15,17,18] and in India [24] to quantify growth responses to various management practices. The Cropping System Model (CSM)-CROPGRO-Peanut is a process-oriented model that is part of the Decision Support System for Agrotechnology Transfer (DSSAT) [6,12,16].
Adapting and evaluating the CROPGRO-peanut model for response to phosphorus on a sandy-loam soil under semi-arid tropical conditions
2015, Field Crops ResearchCitation Excerpt :The model simulates carbon balance, crop and soil N balance, and soil-crop water balance on a daily basis. The model responds dynamically to daily weather inputs and can simulate effects of cultivar choice, crop and soil management practices such as sowing dates, sowing density, irrigation and fertilizer management on groundnut growth, development and yield (Singh et al., 1994; Dangthaisong et al., 2006; Putto et al., 2009). The CROPGRO-peanut model has been evaluated and tested widely for its capability to simulate soil water, growth and yield (Singh et al., 1994; Naab et al., 2004; Dangthaisong et al., 2006).
Effect of Climate Change Factors on Processes of Crop Growth and Development and Yield of Groundnut (Arachis hypogaea L.)
2012, Advances in AgronomyCitation Excerpt :Elevated CO2 does not affect vegetative progression of groundnut (Rao, 1999). Currently in the groundnut model (Boote et al., 1986, 1991, 1998; Singh et al., 1994a,b), the base temperature is 11 °C and the OTs for vegetative development range from 28 to 30 °C, and the damaging threshold temperature is taken as 55 °C. There is little information in the literature on how vegetative development is affected by temperatures above 30 °C.
Analysis of potential yields and yield gaps of rainfed soybean in India using CROPGRO-Soybean model
2008, Agricultural and Forest MeteorologyRegional importance of crop yield constraints: Linking simulation models and geostatistics to interpret spatial patterns
2006, Ecological ModellingCitation Excerpt :To evaluate the impact on the yield gap of changes in environmental conditions, such as those that might be achieved through policy instruments, an understanding of what drives variability in y(u) is needed. Typically, this means obtaining observations of e(u) in farmers fields, which can then be combined with pre-defined models of f (e.g., Aggarwal and Kalra, 1994; Singh et al., 1994; Matthews et al., 2002) or with statistical models relying on joint observations of y(u) to determine the contribution of different factors to yield variability (Calvino and Sadras, 2002; Lobell et al., 2004). While these studies have provided new insights into the yield gap in specific regions, detailed understanding of the causes and often even the magnitudes of yield gaps are poorly known in many regions.