孟加拉湾西南部氮吸收量随环境变量的动态变化

IF 2.9 Q2 GEOGRAPHY, PHYSICAL
Kandasamy Priyanka , Ranjitkumar Sarangi , Vajravelu Manigandan , Durairaj Poornima , Ayyappan Saravanakumar
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Total production ranged between 1.39 and 7.43 mmol N m<sup>2</sup> d<sup>−1</sup>, new production ranged between 0.58 and 2.83 mmol N m<sup>2</sup> d<sup>−1</sup> and regenerated production ranged between 0.83 and 4.59 mmol N m<sup>2</sup> d<sup>−1</sup>. The study observed a significant negative correlation nitrogen uptake along with pH, sea surface salinity (SSS), and sea surface temperature (SST) was observed in the study. The R<sup>2</sup> values for SST were 0.605, 0.619, 0.503, 0.601, and 0.627; for SSS they were 0.688, 0.511, 0.498, 0.579, and 0.644 with nitrogen (Na<sup>15</sup>NO<sub>3</sub>), ammonium (<sup>15</sup>NH<sub>4</sub>Cl), urea (CO(<sup>15</sup>NH<sub>2</sub>)<sup>2</sup>), regenerated, and total production uptake, respectively. pH was highly correlated with nitrate uptake (R<sup>2</sup> = 0.525), had a low correlation with ammonium uptake (R<sup>2</sup> = 0.439) and a moderate correlated with urea uptake (R<sup>2</sup> = 0.526). A positive relationship of nitrogen uptakes with chlorophyll-a, dissolved oxygen, and dissolved inorganic nitrogen (DIN) were observed. Chlorophyll-a had R<sup>2</sup> value of 0.608, 0.126, 0.524, 0.526, 0.578, with Na<sup>15</sup>NO<sub>3</sub>, <sup>15</sup>NH<sub>4</sub>Cl, CO(<sup>15</sup>NH<sub>2</sub>)<sup>2</sup>, regenerated and total production uptake respectively. Dissolved oxygen (DO) related to ammonium uptake showed a very poor correlation (R<sup>2</sup> = 0.079) but a better correlation with urea (R<sup>2</sup> = 0.534). New production uptake rate showed a high positive correlation with DO (R<sup>2</sup> = 0.645), whereas regenerative production uptake rates showed a relatively low correlation (R<sup>2</sup> = 0.519). The positive relationship between DIN and nitrogen uptake had corresponding R<sup>2</sup> value of 0.642, 0.591, 0.558, 0.652 and 0.675 for nitrite, ammonium, urea, regenerated and total production uptakes respectively. 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引用次数: 0

摘要

硝酸盐吸收量是初级生产的基本养分。一项以孟加拉湾(BoB)表层水域为重点的研究,通过硝酸盐、氨和尿素(氮吸收)估算了新产量、再生产量和总产量。沿岸水域的营养限制会干扰环境生物生产力,因此了解沿岸水域的氮吸收率至关重要。需要对这些吸收率和代谢过程进行详细研究,以制定有效的缓解策略,防止这些生态系统进一步退化。总产量介于 1.39 至 7.43 mmol N m2 d-1 之间,新产量介于 0.58 至 2.83 mmol N m2 d-1 之间,再生产量介于 0.83 至 4.59 mmol N m2 d-1 之间。研究发现,氮吸收量与 pH 值、海面盐度(SSS)和海面温度(SST)呈明显负相关。SST 与氮(Na15NO3)、铵(15NH4Cl)、尿素(CO(15NH2)2)、再生氮和总产量吸收量的 R2 值分别为 0.605、0.619、0.503、0.601 和 0.627;SSS 与氮(Na15NO3)、铵(15NH4Cl)、尿素(CO(15NH2)2)、再生氮和总产量吸收量的 R2 值分别为 0.688、0.511、0.498、0.579 和 0.644。pH 值与硝酸盐吸收量高度相关(R2 = 0.525),与铵吸收量相关性较低(R2 = 0.439),与尿素吸收量相关性中等(R2 = 0.526)。氮吸收量与叶绿素-a、溶解氧和溶解无机氮(DIN)呈正相关。叶绿素-a 与 Na15NO3、15NH4Cl、CO(15NH2)2、再生氮和总产量吸收量的 R2 值分别为 0.608、0.126、0.524、0.526 和 0.578。溶解氧(DO)与铵吸收量的相关性很差(R2 = 0.079),但与尿素的相关性较好(R2 = 0.534)。新产量吸收率与溶解氧呈高度正相关(R2 = 0.645),而再生产量吸收率的相关性相对较低(R2 = 0.519)。DIN 与摄氮量之间的正相关关系,亚硝酸盐、铵、尿素、再生摄氮量和总摄氮量的 R2 值分别为 0.642、0.591、0.558、0.652 和 0.675。总氮总磷(TN:TP)与铵呈正相关。在沿海渤海湾,TN:TP 关系非常吻合,R2 = 0.576(硝酸盐吸收量)、0.524(铵吸收量)和 0.503(尿素吸收量)。因此,通过统计分析、主成分分析和皮尔逊相关性分析,证实了提高新产量的环境参数之间的相互依存关系。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Nitrogen uptakes dynamics with environmental variables in the southwest Bay of Bengal

Nitrate uptake is an essential nutrient for primary production. A study focused on the surface waters of the Bay of Bengal (BoB), new, regenerated, and total production were estimated from nitrate, ammonia, and urea (nitrogen uptakes). Understanding nitrogen uptake rates in coastal waters, where nutrient limitations can disturb environmental biological productivity, is essential. A detailed study of these uptake rates and metabolic processes is required to develop effective mitigation strategies to prevent further degradation of these ecosystems. Total production ranged between 1.39 and 7.43 mmol N m2 d−1, new production ranged between 0.58 and 2.83 mmol N m2 d−1 and regenerated production ranged between 0.83 and 4.59 mmol N m2 d−1. The study observed a significant negative correlation nitrogen uptake along with pH, sea surface salinity (SSS), and sea surface temperature (SST) was observed in the study. The R2 values for SST were 0.605, 0.619, 0.503, 0.601, and 0.627; for SSS they were 0.688, 0.511, 0.498, 0.579, and 0.644 with nitrogen (Na15NO3), ammonium (15NH4Cl), urea (CO(15NH2)2), regenerated, and total production uptake, respectively. pH was highly correlated with nitrate uptake (R2 = 0.525), had a low correlation with ammonium uptake (R2 = 0.439) and a moderate correlated with urea uptake (R2 = 0.526). A positive relationship of nitrogen uptakes with chlorophyll-a, dissolved oxygen, and dissolved inorganic nitrogen (DIN) were observed. Chlorophyll-a had R2 value of 0.608, 0.126, 0.524, 0.526, 0.578, with Na15NO3, 15NH4Cl, CO(15NH2)2, regenerated and total production uptake respectively. Dissolved oxygen (DO) related to ammonium uptake showed a very poor correlation (R2 = 0.079) but a better correlation with urea (R2 = 0.534). New production uptake rate showed a high positive correlation with DO (R2 = 0.645), whereas regenerative production uptake rates showed a relatively low correlation (R2 = 0.519). The positive relationship between DIN and nitrogen uptake had corresponding R2 value of 0.642, 0.591, 0.558, 0.652 and 0.675 for nitrite, ammonium, urea, regenerated and total production uptakes respectively. Total nitrogen: Total phosphate (TN:TP) showed a positive correlation with ammonium. The TN:TP relationship fit nicely with R2 = 0.576 (nitrate uptake), 0.524 (ammonium uptake), and 0.503 (urea uptake) in the coastal BoB. Hence, by applying statistical analysis, principal component analysis and pearson correlation, the interdependency of the environmental parameters enhancing the new production has been confirmed.

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来源期刊
Quaternary Science Advances
Quaternary Science Advances Earth and Planetary Sciences-Earth-Surface Processes
CiteScore
4.00
自引率
13.30%
发文量
16
审稿时长
61 days
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