南海北部神狐海域营养盐浓度与结构的分布特征及影响因素

杨建斌; 姚鹏; 张晓华

doi:10.3969/j.issn.0253-4193.2020.10.013

南海北部神狐海域营养盐浓度与结构的分布特征及影响因素

doi: 10.3969/j.issn.0253-4193.2020.10.013

杨建斌^1,,
姚鹏^{1, 2, ,},
张晓华^{2, 3}

详细信息

作者简介:
杨建斌（1994-），男，山东省青岛市人，研究方向为海洋有机生物地球化学。E-mail：913759614@qq.com

通讯作者:
姚鹏（1977-），男，山东省菏泽市人，教授，主要从事海洋有机生物地球化学研究。E-mail： yaopeng@ouc.edu.cn

中图分类号: P714.2⁺2
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出版历程
- 收稿日期: 2020-01-17
- 修回日期: 2020-07-02
- 发布日期: 2020-12-07

The distribution and controlling factors of the concentration and structure of dissolved inorganic nutrients in the Shenhu Area, northern South China Sea

Yang Jianbin^1
,,
Yao Peng^{1, 2
, ,},
Zhang Xiaohua^{2, 3}

摘要

摘要: 生源要素是海洋初级生产的基础，其在海洋环境中的循环受到多种物理、化学和生物过程的影响，对其浓度分布、结构特点及影响因素的认识是理解海洋生态系统动力学的基础。于2019年2月在南海北部神狐海域进行了现场考察和海水样品采集，对海水中的溶解态无机营养盐浓度进行了分析，并结合温度、盐度、叶绿素a(Chl a)、pH和溶解氧(DO)等水文环境参数，研究了神狐海域海水中营养盐浓度与结构的分布特征及影响因素等。在0～30 m的海水中各营养盐浓度均很低，随着深度的增加，营养盐浓度逐渐增大。在水深3 000 m左右处，无机氮、磷酸盐和硅酸盐浓度分别达到了38.02 μmol/L、2.71 μmol/L和149.07 μmol/L。温度、pH和DO与各营养盐浓度均具有显著的相关性，表明环境因素影响着营养盐的生物地球化学过程。此外，在75 m深度，研究区域东北方向的站位营养盐浓度相对较低，并呈现向西南方向逐渐增大的变化趋势，可能与高温、高盐和低营养盐的黑潮水入侵有关。根据端元混合模型计算所得保守混合浓度与实测值的差值显示，在75 m深度硅酸盐和磷酸盐以生物消耗为主，而硝酸盐存在添加。随磷酸盐浓度增加，各站位无机氮浓度呈线性升高，但硅酸盐浓度则以幂函数式升高，表明不同营养盐之间再生速率和再利用效率有所不同。神狐海域的N/P比与Si/N比和Si/P比呈现出截然相反的变化趋势。在0～30 m，N/P比较小而Si/N比和Si/P比较大；在75 m，受不同生物作用影响，N/P比变大，Si/N比和Si/P比变小；在75 m以下N/P比逐渐降低至14.44，而Si/N比和Si/P比则逐渐升高；在1 000 m以下，各营养盐比例均保持稳定。氮异常指数的计算结果显示，神狐海域300 m以上的海水中固氮作用强于反硝化作用，而300 m以下反硝化作用增强。神狐海域营养盐浓度与结构的分布特征表明黑潮入侵和生物活动显著影响了此区域营养盐的生物地球化学过程。
- 神狐海域 /
- 营养盐 /
- 浓度 /
- 结构 /
- 影响因素
Abstract: Biogenic elements are the basis of primary production in marine systems. Their cycles in marine environments are affected by various physical, chemical, and biological processes. Understanding the concentration distribution, structural characteristics, and influencing factors of biogenic elements are essential to understand the dynamics of marine ecosystems. In February 2019, a field investigation was conducted in the Shenhu Area of the northern South China Sea and seawater samples were collected to analyze dissolved inorganic nutrients. Combined with the hydrological environment parameters, such as temperature, salinity, chlrophyll a (Chl a), pH and dissolved oxygen (DO), the distribution and controlling factor of nutrient concentration and structure in the Shenhu Area were discussed. Concentrations of each nutrient in the seawaters from 0 m to 30 m were very low, and the nutrient concentrations gradually increased with the increase of depth. At the depth of about 3 000 m, the concentrations of dissolved inorganic nitrogen (DIN), phosphate and silicate reached 38.02 μmol/L, 2.71 μmol/L and 149.07 μmol/L, respectively. Temperature, pH and DO were significantly correlated with nutrients, indicating that environmental factors greatly affected the biogeochemical processes of nutrients. In addition, the concentration of nutrients in the northeast direction of the study area at a depth of 75 m was relatively low and showed a gradual increasing trend in the southwest direction, which may be related to the intrusion of Kuroshio water with high temperature, high salinity and low nutrients. Meanwhile, the difference between the conservative mixing concentrations calculated based on an end-member mixing model and the measured values of nutrients showed that, at 75 m depth, silicate and phosphate were consumed by biological activities, while nitrates were controlled by biological addition. With the increase of phosphate, the DIN at each site increased linearly, but the silicate increased with a power function, indicating that the regeneration rate and recycling efficiency were different for different nutrients. The ratios of N/P in the Shenhu Area showed opposite trends compared with the ratios of Si/N and Si/P. At 0−30 m, the N/P ratios were low and the Si/N and Si/P ratios were high. At 75 m, the N/P ratios increased along with the decrease of Si/N and Si/P ratios possibly because of different biological effects. Below 75 m, the N/P ratios gradually decreased to 14.44, while the Si/N and Si/P ratios gradually increased. All nutrient ratios remained stable below 1 000 m. The calculation results of the N−anomaly showed that nitrogen fixation in seawater above 300 m was stronger than denitrification, and denitrification below 300 m was enhanced. The distribution characteristics of the concentration and structure of nutrients in the Shenhu Area indicated that the Kuroshio intrusion and biological activities significantly affected the biogeochemical process of nutrients in this area.
- Shenhu Area /
- nutrients /
- concentration /
- structure /
- controlling factors

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图 1 神狐海域2019年2月采样站位（洋流参考文献[12–14]，阴影部分代表神狐海域大致范围^[5]）

Figure 1. Sampling sites in the Shenhu Area in February, 2019 (ocean currents are modified from references [12-14], the shadow area represents the approximate range of the Shenhu Area ^[5])

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图 2 神狐海域水文环境参数和营养盐的垂直分布

Figure 2. Vertical distributions of hydrological parameters and nutrients in the Shenhu Area

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图 3 神狐海域75 m深度水文环境参数和营养盐的水平分布

Figure 3. Horizontal distributions of hydrological parameters and nutrients at 75 m depth in the Shenhu Area

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图 4 神狐海域75 m深度的Δ营养盐（a）和N^*（b）的垂直分布

Figure 4. Δnutrient at 75 m depth (a) and vertical distribution of N^* (b) in the Shenhu Area

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图 5 神狐海域营养盐比例的垂直分布（a. N/P，b. Si/N，c. Si/P，黑色虚线代表Redfield比值^[1]）和75 m深度的水平分布（d. N/P，e. Si/N，f. Si/P）

Figure 5. Vertical distribution of nutrient ratios (a. N/P, b. Si/N, c. Si/P, black dotted line represents the Redfield ratio^[1]) and horizontal distributions of nutrient ratios at 75 m depth (d. N/P, e. Si/N, f. Si/P) in the Shenhu Area

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图 6 神狐海域位温−盐度点聚图

等值线为海水密度σ₀（单位：kg/m³），由ODV软件计算得到。红色正方形代表南海水（14°12′44″N，114°0′47″E），黑色三角形代表黑潮水（18°2′34″N，123°57′32″E），数据源自中国Argo实时资料中心（www.argo.org.cn）；SWM代表南海表层水团；UWM代表南海次表层水团，UIMWM代表南海次–中层混合水团，IWM代表南海中层水团，DWM代表南海深层水团，BBWM代表南海底盆水团

Figure 6. Temperature-Salinity diagrams of the Shenhu Area

The contour line is the seawater density σ₀ in kg/m³, calculated by ODV software. The red square represents the South China Sea water (14°12′44″N, 114°0′47″E), and the black triangle represents the Kurishio water (18°2′34″N, 123°57′32″E), data from China Argo Real-time Data Center (www.argo.org.cn)；SWM represents surface water mass, UWM represents subsurface water mass, UIMWM represents subsurface-intermediate mixed water mass, IWM represents intermediate water mass, DWM represents deep water mass, BBWM represents bottom basin water mass

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图 7 神狐海域营养盐与基础水文参数的相关性（**代表p<0.01）

Figure 7. Correlation between nutrient and hydrological parameters in the Shenhu Area (**: represents p<0.01)

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图 8 神狐海域75 m深度黑潮水比例与营养盐的相关性（**代表p<0.01）

Figure 8. Correlation between nutrients and Kuroshio water fraction at 75 m depth of the Shenhu Area (** represents p<0.01)

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图 9 神狐海域营养盐之间的关系（**代表p<0.01）

Figure 9. Relationships between nutrients in the Shenhu Area (** represents p<0.01)

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表 1 神狐海域中黑潮水比例（%）

Table 1. Kuroshio water fraction in the Shenhu Area (%)

采样深度	SCS002	SCS003	SCS005	SCS006	SCS007	SCS008	SCS009	SCS010	SCS011	平均值
5 m	23.60	14.80	12.23	13.94	11.96	6.91	7.94	9.41	15.84	12.96
30 m	27.40	25.15	3.44	5.94	−	18.30	3.62	1.35	8.01	11.65
75 m	27.18	54.05	9.00	17.33	9.71	26.19	1.96	19.91	3.83	18.80
200 m	−	−	−	−	−	−	−	−	−	−
300 m	−	−	−	−	1.83	−	−	−	1.06	1.44
1 000 m	17.82	11.98	13.61	8.27	7.69	16.46	18.36	4.92	15.05	12.68
底层	−	−	−	−	−	−	−	−	−	−
注：−表示无数据。

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